Colombia - Sedimentary Basins
Content
ANH
AGENCIA NACIONAL DE HIDROCARBUROS
By:
Darío Barrero1 Andrés Pardo2, 3 Carlos A. Vargas2, 4 Juan F. Martínez1
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BAgencia & M Exploration Ltda, Bogotá Nacional de Hidrocarburos (ANH) Universidad de Caldas, Departamento de Ciencias Geológicas, Manizales 4 Universidad Nacional de Colombia, Departamento de Geociencias, Bogotá 2 3
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
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President of the Republic of Colombia
ÁLVARO URIBE VÉLEZ
Minister of Mines and Energy
HERNÁN MARTÍNEZ TORRES
General Director ANH
JOSÉ ARMANDO ZAMORA REYES
Technical Sub-director Sub-direc tor
ROGELIO TORO LONDOÑO
Chief of Geologists
CARLOS A. VARGAS JIMÉNEZ
For information, please contact: AGENCIA NACIONAL DE HIDROCARBUROS – A.N.H.-
Calle 99 No. 9 A - 54 (piso 14) - Bogotá, Colombia Teléfono: Teléf ono: (571) 593 17 17 - Fax: Fax: (571) 593 17 18 www.anh.gov.co [email protected] Línea Gratuita Nacional 018000 953 000
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ISBN: 978-958-98237-0-5 Edited and compiled by: ANH and B&M Exploration Ltda. Copyright © 2007 Printed in Bogotá-Colombia • 2.007
The editor makes no representation, Express or implied, with regard to the accuracy of the information contained in this document and cannot accept any legal responsibility or liability for any errors or omissions that may be made.
Table of Contents Table of Contents
THE NATIONAL NATIONAL HIDROCARBONS AGENCY - A.N.H. MISSION
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VISION
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FUNCTIONS
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GENERAL INFORMATION ABOUT COLOMBIA
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Geographic Location
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Climate
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Population and Language
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Type of Government Government
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2006 Economic Indicators
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Main Imports Main Exports
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1. SEDIMENTARY BASINS OF COLOMBIA: GEOLOGICAL FRAMEWORK
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2. REVIEW OF NOMENCLATURE NOMENCLATURE AND BOUNDARIES OF COLOMBIAN BASINS
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2.1 Brief Historical Overview
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2.2 Colombian Basin Nomenclature and Boundaries
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2.3 Proposed Modications to the Sedimentary Basin Map of Colombia
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2.4 Proposed Boundaries
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3. PETROLEUM GEOLOGY OF COL COLOMBIAN OMBIAN BASINS
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3.1 Caguán - Putumayo
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3.2 Catatumbo
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3.3 Cauca-Pa Cauca-Patía tía
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3.4 Cesar- Ranchería
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3.5 Chocó
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3.6 Eastern Cordillera
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3.7 Eastern Llanos
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3.8 Guajira
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3.9 Guajira Offshore
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3.10 Los Cayos Basin
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Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
3.11 Lower Magdalena Valley
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3.12 Middle Magdalena Valley
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3.13 Sinú-San Jacinto
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3.14 Sinú Offshore
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3.15 Upper Magdalena Valley
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Figures Figure 1. Official map of terrestrial terres trial and maritime mari time frontiers frontie rs of colombia
(IGAC, 2002)
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Figure 2. Map of Colombia showing its three main tectonic domains.
1) Eastern Region; 2) Central Region; 3) Western Western Region (explanation in the text).
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Figure 3. Classication of sedimentary basin in Colombia
(ECOPETROL, 2000) and adopted in the ANH land map
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Figure 4. Proposed basin map of Colombia for ANH 2007.
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Figure 5. Bathymetric map of the eastern Pacic Ocean and the
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Caribbean Sea and location of the Los Cayos (14), Colombia (08) and Colombian Deep Pacic (09) basins.
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Figure 6. Amagá Basin (01), location and boundaries.
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Figure 7. Caguán - Putumay Putumayo o Basin (02), location and boundaries.
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Figure 8. Catatumbo Basin (03), location and boundaries.
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Figure 9. Cauca-Patía Basin (04), location and boundaries.
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Figure 10. Cesar-Ranchería Basin (05), location and boundaries.
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Figure 11. Chocó Basin (06), location and boundaries.
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Figure 12. Chocó offshore Basin (07), location and boundaries.
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Figure 13. Eastern Cordillera Basin (10), location and boundaries.
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Figure 14. Eastern Llanos Basin (11), location and boundaries.
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Figure 15. Guajira Basin (12), location and boundaries.
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Figure 16. Guajira offshore Basin (13), location and boundaries.
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Figure 17. Los Cayos Basin (14), location and boundaries (see
also the gure 4).
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Figure 18. Lower Magdalena Valley Basin (15), location and boundaries.
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Figure 19. Middle Magdalena Valley Basin (16), location and boundaries.
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Figure 20. Sinú –San Jacinto Basin (17), location and boundaries.
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Figure 21. Sinú Offshore Basin (18), location and boundaries.
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Figure 22. Tuma Tumaco co Basin (19), location and boundaries.
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Figure 23. Tuma Tumaco co Offshore Basin (20), location location and boundaries. boundaries.
Figure 24. Upper Magdalena Valley Basin (21), location and boundaries.
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Figure 25. Urabá Basin (22), location and boundaries.
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Figure 26. Vaupés – Amazonas Basin (23), location and boundaries.
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Figure 27. Caguán – Putumay Putumayo o Petroleum system chart.
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Figure 28. Catatumbo Petroleum system chart.
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Figure 29. Cauca – Patía Petroleum system chart.
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Figure 30. Cesar – Ranchería Petroleum system chart.
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Figure 31. Eastern Cordillera Basin Petroleum system chart.
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Figure 32. Eastern Llanos Basin Petroleum system chart.
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Figure 33. Guajira Basin Petroleum system chart.
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Figure 34. Lower Magdalena Valley Basin Petroleum system chart.
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Figure 35. Middle Magdalena Valley Basin Petroleum system chart.
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Figure 36. Sinú – San Jacinto Basin Petroleum system chart.
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Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
MISSION •
The ANH is the agency responsible for promoting the optimal exploitation of the country’s hydrocarbons resources, by managing them integrally and nding a balance between the interests of the State, Colombian society and companies operating in the sector.
VISION
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The ANH will be recognized recognized as a world world model institution because because of: •
Its knowledge of the Colombian sub-surface potential and the maximization of its exploitation;
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The efficienc ciencyy in the management of hydrocarb hydrocarbons ons and the joint work with both industry and the community; and
•
The professionalism of its team, a high technological level and its efficienc ciencyy and exibility exibilit y in key processes.
FUNCTION •
Manage the nation’s hydrocarbons areas and assign them for exploration
and production. Assess the country’s country ’s hydrocarbons hydrocarbons potential. • Sign and manage new hydrocarbons exploration and exploitation contracts. • Design, evaluate and carry out strategies for the promotion of the country’s hydrocarbons areas. • Support the Ministry of Mines and Energy in the formulation of government policy for the sector. • Manage and preserve technical information, both currently existing and acquired in the future. • Negotiate, as part of the contracts, the terms and conditions of programs that will be carried out by the contractors in benet of communities in the areas of inuence of the contracts. c ontracts. •
Manage the State’s share in exploration and exploitation contracts.
• Manage and dispose of the assets that become property of the State when concessions nish or revert. • Collect royalties and nancial resources that belong to the State for the exploitation of hydrocarbons, and make payments to entities entitled to those resources. • Retain the sums corresponding to shares and royalties that belong to participating entities, which are channeled to the Petroleum Savings and Stabilization Fund (FAEP), (FAEP), and arrange the corresponding drafts and refunds. • Undertake necessary steps to ensure an adequate supply of hydrocarbons,, derivates and products, to meet national demand. hydrocarbons • Fix oil production levels in concession that exploiters must sell for domestic rening. • Fix the price for crude oil in concession sold for domestic rening, processing or for use within de country, as well as for natural gas effectively used as raw material in petrochemical industrial processes, when necessary. • Carry out all other activities in relation with the management of hydrocarbons owned by the nation, as well as those established by law or regulations, in line with the Agency’s mandate. mandate. • Decree 1760 has more detailed information about Ecopetrol’s restructuring and the organizational structure of the National Hydrocarbons Agency.
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GENERAL INFORMATION ABOUT COLOMBIA
Geographic Location The Republic of Colombia Colombia is strategically located in the north-western north-western corner or South America, with an area of 1.14 million square kilometers. It is the only South American country with two coasts, the Pacic (1,300 km) and the Atlantic (1,600 km) (gure 1).
Climate Colombia’s diverse topography produces a variety of climates, ranging from hot to perpetual snows. In general, the coastal and Amazonian areas are warm and tropical, while the mountainous terrain in the center of the country is cool throughout the year.
Population and Language The population was almost 42 million in 2005, with 75% concentrated in urban centers and growing at 2.21% a year (http://www.dane.gov. (http://www.dane.gov.co/censo/). co/censo/). There are more than 33 towns with wit h over 100,000 100,0 00 inhabitants inhabit ants each. each . The official language langu age is Spanish but English is widely used in business circles.
Type of Government Colombia is a democratic republic with a President heading the executive branch, and a legislative branch made up by the Senate and the House of Representatives, with 112 and 199 members respectively. All are elected by popular vote for a four-ye four-year ar period.
2006 Economic Indicators GNP per capita US$ 3.083 Annual Ination 4.48% Foreign Foreig n Investment MUSS 6000 Growth Intern Brute Product 5.96%
Main Imports Machinery, chemicals, metals, transport equipment, minerals, plastics and papers.
Main Exports Oil, coal, nickel, coffee, bananas, owers, cotton, sugar, fruits, minerals, chemicals, and textiles.
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Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
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Figure 1. Offi cial map of terrestrial and maritime frontiers of Colombia (IGAC, 2002).
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
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Andrés Pardo1, 3 Darío Barrero2 Carlos A. Vargas1, 4 Juan Fernando Martínez2
Agencia Nacional de Hidrocarburos (ANH) B & M Exploration Ltda, Bogotá Universidad de Caldas, Departamento de Ciencias Geológicas, Manizales 4 Universidad Nacional de Colombia, Departamento de Geociencias, Bogotá 1 2 3
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From Paleozoic to Late Cenozoic, the basins of Colombia have undergone changes in direction and shape due to different events of rifting and oblique collisions followed by transpression and transtensional tectonics deformation. As a consequence the tectonic evolution of most, if not all, Colombian basins should be considered as poly-history. From a structural/stratigraphic perspective, our knowledge varies greatly from basin to basin. This complicates comparison, especially where an author has emphasized only one aspect of the t he basin evolution. The northwestern corner of South America, where Colombia is located, has experienced different geologic events that controlled the distribution, genesis, basin ll and bounding structures of the sedimentary basins. In this chapter, the chronology of the main geologic phenomena that occurred in the country are sketched, emphasizing those that generated sedimentary deposits that, nowadays,, constitute source rocks, reservoir rocks, sealing units and overburden nowadays sequences and nally hydrocarbon traps. In order to describe these events it is necessary to point out that Colombia can be divided in at least three main tectonic domains: 1) The Eastern region limited on the west by the foothills of the Eastern Cordillera (gure 2). It consists of a Paleozoic and Precambrian basement with a Paleozoic-Cenozoic sedimentary cover that has undergone mild deformation; 2) The Central region comprises the Eastern Cordillera, Sierra Nevada de Santa Marta, the Magdalena River valley and the Central Cordillera extending as far as the Romeral fault system to the west (Figure 2) (San Jerónimo and CaucaAlmaguer faults of the Ingeominas Map, 2006). A sedimentary-metamorphic cover rests on a Grenvillian basement believed to be accreted to the South American border during Paleozoic time; 3) The Western region located, at the west of the Romeral fault system (Figure 2), composed of Mesozoic-Cenozoic oceanic terranes accreted to the Continental margin during Late Cretaceous, Paleogene and Neogene. Lower Paleozoic marine and coastal siliciclastic and carbonate sediments, are distributed throughout the Eastern region (Llanos Basin) and extend into the Central region (Upper Magdalena Valley. Mojica et al., 1988; Trumpy, Trumpy, 1943). These deposits are very fossiliferous which range from Middle Cambrian to Llanvirnian in age. Trilobites, brachiopods, brachiopods, and graptolites in gray to black shales are reported from outcrops in the Upper Magdalena Valley and in many wells drilled in the Llanos basin. In some places, the thermal maturity of these Lower Paleozoic sequences indicates appropriate conditions for hydrocarbon generation. Dated Lower Paleozoic Paleozoic intrusives outcrop along the Eastern Cordillera and Upper Magdalena basins of the Central region (Etayo-Serna et al., 1983; Forero-Suarez, 1990, Maya, 1992). These intrusives crosscut a low grade metamorphic sequence
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Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
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Figure 2. Map of Colombia with its main tectonic domains. 1) Eastern Region;
2) Central Region; 3) Western Region (explanation in the text). In red: regional faults (see the gure 3 for nomenclature). Gray and shadow areas: Main mountain ranges. R.F.S. Romeral fault system; S.N.S.M. Sierra Nevada de Santa Marta. Deep marine and Los cayos basins are not included.
and are overlain by Upper Paleozo Paleozoic ic sedimentary rocks. Folding, Folding, metamorphism and granitic intrusions are probably the result of eastward directed subduction. This regional tectonic event is known k nown as the Caparonensis Orogeny (RestrepoPace, 1995; Barrero and Sanchez, 2000; Aleman and Ramos, 2000). The sedimentary sequences in this area consist of marine black shales and continental red-beds of Devonian age. In some places, this continental Devonian is followed by an Upper Carboniferous (Pensylvanian) consisting of limestones, conglomerates, sandstones and graphitic shales with abundant marine fauna. Permian rocks are absent in the southern portion of the Central region. However, farther to the north in the Santander Massif, Serranía de Perijá and Sierra Nevada de Santa Marta, fossiliferou fossiliferouss limestones of Lower Permian age have been reported. Folding and granitic intrusions related to shear zones might represent oblique collision and accretion of Upper Paleozoic rocks during formation of the Pangea supercontinent. Development of most of the Colombian sedimentary basins begins in the Late Triassic Tria ssic (Rolón et al., 2001; Barrero Barrero,, 2004) during the break break-up -up of Pan Pangea. gea. Early Jurassic to Lower Cretaceous sediments were deposited in a northwest-southeastnortheast trending highly irregular rift ri ft system now underlying the Upper Cretaceous to Neogene sedimentary cover (Etayo et al., 1976; Fabre, 1983; Barrero, 2000; Rolón et al., 2001). The post-rift phase of the system is characterized by the formation of a widespread sag due to the thermal subsidence that together with a global eustatic sea level changes during Middle Albian and Turonian times give origin to organic-matter-rich sediments of the t he Simiti-Tablazo, Simiti-Tablazo, Tetúan and La Luna source rocks responsible for generating the most of the hydrocarbon found in Colombia. The Late Cretaceous-P Cretaceous-Paleogene aleogene exhumation of the Central Central and Eastern cordilleras was linked to the oblique accretion of oceanic rocks (e.g. Western Cordillera basement); as a result a transition from marine, nearshore to continental sedimentary deposits took place. Growth unconformities and uvial siliciclastic sequences on top of them characterize the Paleogene and Neogene sedimentary ll. These uvial deposits contain most of the hydrocarbon reserves of Colombia. The Neogene period is characterized by intense volcanic activity in the western edge of the Central Region (Central Cordillera), linked to a collisional event. As a result, the uvial deposits of the intermontane basins east and west of the Romeral fault system are rich in volcano-clastics (e.g. La Paila, Combia, Honda and Mesa formations). These thick molassic deposits represent the overburden sequences to most of the Petroleum systems of the Colombian basins. Initial basin geometry in Colombia was drastically modied by the Campanian and Miocene collisional events. The Campanian-Maastrichtian collision of the oceanic rocks to the west gave rise to development of the Colombian forelandbasin system (Barrero, 2004; Gómez et al., 2005). By Early Miocene, a second major transpressional event produced by collision of the Central America Island Arc, break-apart the widespread foreland basin system given origin to a number of broken-foreland broken-forelan d basins (intermontane). This nal conguration is what is portrait in the sedimentary basins map of Colombia (gure 4). The Western Region, located west of the Romeral fault system, is composed of mac and ultramac rocks, deep-water siliceous shales, turbidites and
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Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
minor carbonates, in stratigraphic relationship poorly know so far. The tectonic complexity of this region has lead to some authors to use the term complex for units composed of volcanic sedimentary rocks (Maya and Gonzalez, 1995; Moreno-Sanchez and Pardo-Trujillo Pardo-Trujillo,, 2003). Indeed, some of these complexes are collage of sedimentary/tectonic units highly deformed during oblique collisional events. The igneous rocks of these complexes consist of Cretaceous basalts of oceanic crust, plateau (Nivia, 1989) and island arc origin incorporated in a west-verging thrust system with right-lateral strike slip component. The basaltic units are intruded by plagiogranites, gabbros, ultramac rocks and cuarzodiorite stocks (Barrero, 1979; Nivia, 1989). These complexes are covered by Paleogene-Neogene volcanics and mollasic deposits. By Campanian-Maastrichtian time sequence of turbiditic sandstones, siliceous mudstone, calcareous sandstones and black and green shales rich in organic matter is know as the Nogales Formation (Nelson, 1957; Pardo et al., 1993). The Nogales Formation is believed to be the source rock for the oil seep present in the Patía sub-basin (Barrero-Lozano et al, 2006; Rangel et al., 2002) (Figure 4). The entire Western Western Region is considered to be composed of a still unknown number of allocthonous terranes by most of the geoscientists that had worked in that part of Colombia (e.g. Toussaint, 1996). The general
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agreement is that the Western Region is part of the Caribbean plate that moves during Late Cretaceous from a Pacic Ocean location to its present position. The precise dynamics and kinematics of this paradigm are still poorly understood and probably will remain so far for a long time. An important conclusion of the assumed displacement and diachronous oblique collision of the Western Region against the Continental margin of Western Colombia is the need for new kinematic models to explain deformation of the Central and Eastern Regions. As to day, the most plausible kinematic model to explain deformation of the northern Andes is one of dextral transpresion/ transtension system as postulated by Montes, Hatcher and Restrepo-Pace (2005).
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
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Andrés Pardo1, 3 Carlos A. Vargas1, 4 Darío Barrero2 Juan Fernando Martínez2
Agencia Nacional de Hidrocarburos (ANH) B & M Exploration Ltda, Bogotá 3 Universidad de Caldas, Departamento de Ciencias Geológicas, Manizales 4 Universidad Nacional de Colombia, Departamento de Geociencias, Bogotá 1 2
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2.1 Brief Historical Overview Petroleum production production in the country began in 1921 with the granting of the Barco and De Mares concessions, which included the jungle regions of Catatumbo at the Venezuelan frontier and those of Opón - Carare, in the Middle-Magdalena. Middle -Magdalena. ECOPETROL was authorized by the government since 1969 to work lands other than those of the former De Mares Concession (Barco and Infantas or Catatumbo and VMM). In I n 1974, Colombia began using the Association Contract system, which became an important tool in hydrocarbon exploration, through the addition of private capital (domestic and foreign), in association with ECOPETROL. In 1985, Govea and Aguilera, ECOPETROL employees, published an article describing 13 sedimentary basins for Colombia. According to the authors, authors, their origin is related to Andean orogeny, and they used the classication of Kingston et al. (1983), as a basis. Three groups were were recognized: • Continental Basins: Eastern Llanos, Putumay Putumayo, o, Mid-Magdalena Valley, Upper Magdalena Valley, Valley, Catatumbo, Cesar – Ranchería, Sabana de Bogotá, Amazon and Los Cayos • Continental borderland Basins: Lower Magdalena Valley and Guajira. • Oceanic Basins: Chocó - Pacic and Cauca - Patía. Subsequent to this proposal, ECOPETROL (2000) presented a map with a subdivision of 18 basins, which was adopted by the ANH (gure 3). Given that, to our knowledge, there the re is no official document indicatin in dicating g in detail the geological geologic al and/or geographical characteristics used to delimit these basins, the technical assistant directorate of the ANH is setting forth a proposal to review the nomenclature and boundaries of the Colombian sedimentary basins presented in this document.
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Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
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Figure 3. Classication of sedimentary basins in Colombia (ECOPETROL, 2000) and adopted in the ANH land map (http://www.anh.gov.co/html/i_portals/inco/html/i_portals/in-
dex.phz).
2.2 Colombian Basin Nomenclature and Boundaries The nomenclature and boundaries of the Colombian Sedimentar Sedimentaryy basins as they appear in the ANH land map need some clarication based on geological and/or planning and operation criteria for exploration activities activitie s in the petroleum industry. It is important to mention that some of these regions do not strictly meet the denition of a sedimentary basin, given that they correspond to areas which have undergone different geological events over time. They could be best dened as Geologic Provinces which, accordingly with the USGS (2000): “each geologic province is an area having characteristic dimensions of perhaps hundreds to thousands of kilometers encompassing a natural geologic entity (for example, sedimentary basin, thrust belt, delta) or some combination of contiguous geologic entities” and their limits are drawn along natural geologic boundaries or, in some cases, at an arbitrary water deep in the oceans. Nevertheless, the term sedimentary basin is conserved conser ved here because it is deep-rooted in the geological literature of Colombia. The new proposal divides the Colombian territory in 23 sedimentary basins (gure 4 and 5): 1. Amagá 2. Caguán-Putumayo 3. Catatumbo 4. Cauca-Patía 5. Cesar-Ranchería 6. Chocó 7. Chocó Offshore 8. Colombia 9. Colombian Deep Pacic 10. Eastern Cordillera 11. Eastern Llanos 12. Guajira 13. Guajira Offshore 14. Los Cayos 15. Lower Magdalena Valley 16. Middle Magdalena Valley 17. Sinú-San Jacinto 18. Sinú Offshore 19. Tumaco 20. Tumaco Offshore 21. Upper Magdalena Valley 22. Urabá 23. Vaupés-Amazonas
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Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
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Figure 4. Proposed basin map of Colombia for ANH 2007.
2.3 Proposed Modications to the Sedimentary Basin Map of Colombia It is proposed to include the Amagá Basin in the Antioquia region. Despite its low prospectiveness for conventional hydrocarbon exploration, the sedimentary rocks in this region are rich in organic material and coal, which must be evaluated for hydrocarbon hydrocarbon extraction by non-conventional non-conventional methods. The northern limit of the Guajira Offshore and Sinú Offshore basins were extended to the South Caribbean Deformed Belt deformation front (gure 4). The Basin called “Pacíco “Pacíco”” in the basin map of of the ANH was included included among the “economic “econ omic basement”, basement”, as it corresponds for the most part par t to basic igneous rocks of the Baudó Mountain Range. Thus, the new onshore basins of the Pacic area would be divided into the Chocó basin to the north and the Tumaco basin to the south, separated by the Garrapatas fault zone (gure 4). Two deep marine basins are included in this proposal: the Colombian Basin in the Caribbean and the Colombian Deep Pacic Basin in the Pacic Ocean which are mainly limited by international maritime boundaries (gure 5). In the region that includes the Putumayo, Caguán-Vaupés and Amazon basins (gure 3), it is proposed that it be separated into two prospective areas (gure 4): 1) The Vaupés-Amazonas Vaupés-Amazonas basin, which corresponds to an elongated depression extending from the east margin of the Eastern Cordillera, down southeast to the Amazon River. The The eastern and western boundaries of this basin correspond to structural high grounds composed of Paleozoic rocks (e.g. Chiribiquete mountain range to the W and La Trampa mountain range, Diamaco and Circasia hills and Carurú plateau to the E; gure 4). According to its morphology and gravimetric information, this basin corresponds to a graben which could be a prolongation prolongation to the north of the Solimoes Basin. 2) The Caguán-Putumay Caguán-Putumayo o Basin: it is proposed to extend the former Putumayo Basin to the western edge of Chiribiquete structural high ground (gures 3 and 4). The Paleozoic rocks of the subsurface could present prospectiveness, considering that, to the south, in the Peruvian Basin of Marañón, important hydrocarbon reserves have been discovered in rocks of this age.
2.4 Proposed Boundaries The objective of this chapter is to introduce the t he user in a new proposal about the boundaries of the sedimentary basin of Colombia, as they are described by geoscientist of the ANH (gures 4 and 5). It should be taken in consideration the great difficulty in i n dening boundaries bo undaries for basins with a poly-histor poly -historic ic development, as it is the case for most of the Colombian sedimentary basin.
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Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
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Figure 5. Bathymetric map of the eastern Pacic Ocean and the Caribbean Sea
and location of the Los Cayos (14), Colombia (08) and Colombian Deep Pacic (09) basins. Limits are mainly based on the official map of the Colombian maritime boundaries (IGAC, 2002). H.E. Hess Escarpment; C.P.S.Z. Colombian Pacic Subduction Zone; S.C.D.B. South Caribbean Deformed Belt deformation front; N.P.D.B. North Panama Deformed Belt deformation front. Map modied from Niitsuma et al. (2006).
Amagá Basin
The Amagá Basin is a collision-related basin, formed to the west of the Romeral fault system. It covers an area located in the southwest of the Departamento de Antioquia and the northern edge of Departamento de Caldas (gures 1 and 4). The west and east limits of this basin are the Cretaceous igneous and sedimentary rocks of the Central and Western cordilleras and partially regional faults (gure 6). It consists of uvial deposits with important coal layers buried by Neogene volcanoclastics, tuff and lava ows. This small basin could be an important exploration target for coal-bed methane.
Caribbean aribbeanSea Sea
P N M VENEZUEL
Pacific acificOcean Ocean COLOM
I
Medellin
ECU
R ZIL
DOR
PERU
n a e c c O c c i f i c a P
1
S . F . C
S . F . R
Bogotá
BOUNDARIES East: Cretaceous igneous-sedimentary rocks (Central Cordillera) West: Cretaceous volcanic and sedimentary rocks (Western Cordillera) R.F.S. R.F .S. Romeral fault system C.F.S. C.F .S. Cauca fault system
Figure 6. Amagá Basin (01), location and boundaries.
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Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
Caguán - Putumayo Basin
This new-named basin is the northernmost extension of the Oriente-Marañon basin. In this document it is proposed to extend the limits of the Putumayo basin to include the area of the Caguán sedimentary section, taken in consideration the presence of a prospective Paleozoic Paleozoic section as such found in Perú. The limits of this basin are: the Eastern Cordillera foothills thrust system to the northwest; the Macarena structural high to the northeast; the Ecuadorian and Peruvian international border to the south and a structural high to the east, which includes the Serranía de Chiribiquete (gure 7). General information: Higley, 2001; Mathalone and Montoya, 1995.
BOUNDARIES 32
Northwest: Eastern Cordillera foothills fault system East: Structural high, including the Serranía de Chiribiquete (SCH) South: Ecuadorian-Peruvian International border Northeast: Sierra de la Macarena (SM)
Figure 7. Caguán - Putumayo Basin (02), location and boundaries.
Catatumbo Basin
The Catatumbo Basin is the Colombian portion of the Maracaibo Basin, a petroleum supergiant basin that accounts for about two percent (2%) of the hydrocarbon reserves of the world. Its north and east limits are the geographic border with Venezuela; to the south the limit is with outcropping Cretaceous rocks of the Eastern Cordillera and, to the west the igneous and metamorphic rocks of the Santander massif (gure 8). General information in: Mann et al., 2006; Talukdar and Marcano, 1994; Yurew Talukdar Yurewicks icks et al., 1998, Alfonso and Mondragón, 2000.
BOUNDARIES 33
North: Geographic Border with Venezuela South: Eastern Cordillera Cretaceous rocks West: Santader Massif igneous and metamorphics East: Geographic Border with Venezuela
Figure 8. Catatumbo Basin (03), location and boundaries.
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
Cauca-Patía Basin
This Cenozoic collision-related basin is bounded to the north and south by basic igneous rocks of Late Cretaceous age. Its eastern and western limits are regional tectonic features (gures 4 and 9). The eastern limit is partially dened by the Romeral fault system, which separate continental crust to the east from oceanic crust to the west. General information in: Barrero et al., 2006; Barrero, 1979; Barrero and Laverde, 1998; Aleman and Ramos, 2000; Rangel et al., 2002; Moreno-Sánchez and Pardo-Trujillo, 2003.
BOUNDARIES
34
West: Cauca fault system (C.F (C.F.S.), .S.), Western Cordillera volcanic and sedimentary rocks (23) East: Romeral fault system (R.F.S.), Central Cordilera (22) North and South: Cretaceous basic igneous rocks
Figure 9. Cauca-Patía Basin (04), location and boundaries.
Cesar-Ranchería Basin
This intermontane (broken-forelan (broken-foreland) d) basin is bounded to the northwest by the Pre-Cretaceous rocks of the Sierra Nevada de Santa Marta. The northeast limit is the sharp trace of the Oca fault; to the east-southeast the limit is the pre-Cretaceous rocks of the Serranía de Perijá and the Colombian-Venezuelan boundary, and to the southwest the trace of the Bucaramanga fault (gure 10). This basin has a general orientation N30°E and, and, the Verdesia Verdesia high divides divides it in the southern Cesar and the northern Ranchería sub-basins.
BOUNDARIES SW: Bucaramanga-Santa Marta Fault (B.S.M.F)
35
E-SE: Pre-Cretaceous rocks of the Serranía de Perijá (22); Colombian-Vene Colombian-Venezuelan zuelan boundary. NE: Oca Fault (O.F.) NW: Pre-Cretaceous rocks of the Sierra Nevada de Santa Marta (23)
Figure 10. Cesar-Ranchería Basin (05), location and boundaries.
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
Chocó Basin
This basin has been interpreted as the product of extension ex tension in a forearc setting. The north-northwest limit of the basin is the geographic boundaries with Panamá; to the northwest the basin sediments lap on the basaltic complex of the Serranía de Baudó; the southwest limit is the present Pacic coastal line; the east limit is the quartzdioritic Mandé batholith the Cretaceous rocks of the Western Cordillera and partially, the Murindó fault. The Garrapatas fault zone, a NNE trending shear zone, marks the south limit of the basin (gure 11). This sedimentary area has been subdivided in two basins for some authors (e.g. Duque-Caro, 1990): the Atrato Basin to the north and the San Juan Basin to the South divided by the Itsmina fault zone. General information: Barrero, 1979; Geotec, 1988; Duque-Caro, 1990; Aleman and Ramos, 2000; IGAC-Ingeominas, 2001.
36
BOUNDARIES N-NW: Geographic border of Panamá South: Garrapatas fault zone (G.F (G.F.Z.) .Z.) NW: Serranía de Baudó (SB) SW: Present Pacic coastline East: Mande quartzdiorite (M.B.), the Cretaceous rocks of the Western
Cordillera (WC ) and partially the Murindó fault (M.F (M.F.).)
Figure 11. Chocó Basin (06), location and boundaries.
Chocó Offshore Basin
The Chocó Offshore Basin is located along the arcuate corner of northwestern Colombia, south of the Panama border, under waters of the Pacic Ocean. This offshore basin extends from the west of the present coastal line as far as the trench of the present subduction zone. To To the north the basin limit is the Panama border, and to the south the limit is roughly the trace of the Garrapatas fault system (gure 12). General information: IGAC-Ingeominas, 2001; Ingeominas, 2006; Geotec, 1988.
BOUNDARIES NNE: Geographic border of Panama
37
South: Garrapatas fault zone (G.F.Z.) (G.F.Z.) West: Trench of the present subduction zone (S.Z.) East: Present coastal line
Figure 12. Chocó offshore Basin ( 07), location and boundaries.
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
Colombia Basin
The Colombian Basin is a deep water basin located in the Caribbean Sea. Its northwestern limit is considered here the Hess Escarpment, a major feature extending from eastern Central America to Hispaniola (Figure 5). The southwestern southwestern limit of this basin is the Costa Rica and Panama maritime boundaries, the southeastern limit is located in the South Caribbean Deformed Belt deformation front; the eastern boundary is the maritime Colombian-Venezuelan Colombian-Venezuelan frontier, and the northern limit is the Jamaica, Haiti and the Dominican republic maritime boundaries (gures 4 and 5). Due to the petroleum geology of this basin is still unknown; it is not mentioned in the next section of this book. General information: Mann, 1999.
Colombian Deep Pacic Basin
38
This name is proposed here to include the westernmost marine basin of Colombia, which is mainly composed by oceanic volcanic rocks and deep marine sediments. Its northern limit is located in the Colombian-Panama maritime boundaries; the western limit is placed in the Colombian-Costa Rica boundary; to the south it is bounded by the Colombian-Ecuad Colombian-Ecuadorian orian marine boundary. To the east the basin is limited by the Colombian Pacic Subduction Zone (gure 5).
Eastern Cordillera Basin/Fold belt
The Eastern Cordillera basin is composed by rocks formed in an inverted Late Triassic rift system that resulted from the break-up break-up of Pangea Pangea (Rolón et al., 2.001) and was lled by Mesozoic marine and Cenozoic continental sediments. By Early Paleogene a dextral transpressional deformation triggered faulting and folding and played a fundamental role in the structural inversion of this basin. As a consequence of its origin and structural development the present day limits of the basin are very ve ry irregular irr egular and diffi cult to describe. descr ibe. In a general gener al way, east and west limits are well developed en-echelon faults that thrust-over the adjacent basins, the eastern limit is known as the frontal thrust system of the Eastern Cordillera; the western limit are the Bituima and La Salina fault systems (Llinas, J.C., 2.001, La Luna Oil, Internal report). The southeast boundary is the AlgecirasGarzón dextral strike-slip fault system, and the northern limit the igneous and
metamorphic rocks of the Santander massif (gure 13). The eastern portion of the basin is the well-known Llanos Foothills. General information: Casero et al., 1997; Montes, et al., 2005; Gómez, et al., 2005; 2005 ; Rolón, et al., 2001; Kammer, K ammer, 1999; RestrepoPace, 1989; Restrepo-Pace, Restrepo-Pace, 1999; Dengo and Covey, 1993; Julivert, 1958; Fabre, 1985.
BOUNDARIES North: Igneous and metamorphic rocks from the Santander massif (S.M.) South: Algeciras-Garzón fault system (A.G.F.S.) 39
West: Bituima and La Salina fault systems (B.S.F (B.S.F.S.) .S.) East: frontal thrust system of the Eastern Cordillera
Figure 13. Eastern Cordillera Basin (10), location and boundaries.
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
Eastern Llanos Basin
The Eastern Llanos Basin is the most prolic hydrocarbon basin in continental Colombia. The northern limit of this basin is the Colombian-Venezuelan border; to the south the basin extend as far as the Macarena high, the Vaupés Arch and the Precambrian metamorphic rocks that outcrops to the south of the Guaviare river; the eastern limit is marked by the outcrops of Precambrian plutonic rocks of the Guyana Shield and to the west the basin is limited by the frontal thrust system of the Eastern Cordillera (gure 14). General information: Casero et al.,1997; Gómez et al., 2005; Etayo-Serna et al., 1983; 1983 ; Cooper et al., 1995.
BOUNDARIES 40
North: Geographic Border Venezuela South: Serranía de la Macarena (SM), Vaupés Arch (VA), and Precambrian metamorphic rocks (PM) West: frontal thrust system of the Eastern Cordillera East: Guyana Shield Precambrian rocks (GS)
Figure 14. Eastern Llanos Basin (11), location and boundaries.
Guajira Basin
The Guajira Basin is located in the northernmost region of Colombia. The north, northwest and northeast limits of the basin are the present Caribbean coastline; the southeast limit is the geographic boundary with Venezuela; the southern limit is the trace of the Oca fault (gure 15). The basin has been divided by the trace of the Cuiza fault into Upper Guajira and Lower Guajira sub-basins. From a kinematic point of view, the Lower Guajira is here considered a geologic feature formed as a consequence of a releasing step-over in a transtensional environment of the Oca-Cuisa fault system. General information: Barrero-Lozano, 2004; Geotec, 1988; Ingeominas, 2006; Mann, 1999.
BOUNDARIES
41
North and Northwest: Caribbean shoreline Northeast: Caribbean shoreline South: Oca Fault (O.F.) Southeast: Colombia-Venezuela border
Figure 15. Guajira Basin (12), location and boundaries.
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
Guajira Offshore Basin
The northern-northwestern limit of this basin is the South Caribbean Deformed Belt deformation front originated by the interaction between the South American and the Caribbean Plate; to the east the limit is the geographic line dening the Colombia-Venezuela border; to the southwest the basin goes as far as the offshore trace of the Oca fault and to the Southeast the continental Guajira shoreline (gure 16). General information: Cediel et al., 1998; Geotec, 1988; Ingeominas, 2006; Mann, 1999.
BOUNDARIES 42
North-Northwest: South Caribbean Deformed Belt deformation front (S.C.D.B.) Southwest: Oca Fault (O.F.) Southeast: Continental Guajira shoreline East: Colombia-Venezuela border
Figure 16. Guajira offshore Basin (13), location and boundaries.
Los Cayos Basin
Los Cayos Basin is an oceanic basin within the Caribbean Sea region. The north and western limits of this basin are the international boundaries (gures 5 and 17); the east southeastern limit is considered here the Hess escarpment (gure 5) which separates the Nicaraguan Rise to the norhwest and the Colombian basin to the Southeast. The basin ll consist of a Paleogene carbonate-siliciclastic sequence followed by Neogene siliciclastics. Basement rocks are Cretaceous siliceous deposits and basalts.
BOUNDARIES 43
North, East and West: International boundaries South-Southeast: Hess Escarpment (H.E.)
Figure 17. Los Cayos Basin (14), location and boundaries (see also the gure 4).
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
Lower Magdalena Valley Basin Lower Magdalena Valley Basin (LMVB)
The Lower Magdalena Valley Basin (LMVB) is a triangular transtensional basin bounded to the west and north by the Romeral fault system and to the south and south-east by the metamorphic and igneous complex of the Central Cordillera and the Serranía de San Lucas, a boundary that seems to be a major strike-slip fault system (Espíritu Santo fault system). The eastern limit of the basin is the northern portion of the Bucaramanga-Santa Marta fault system (gure 18). A basement high divides the basin into the northern El Plato and the southern San Jorge sub-basins. General information: Ingeominas, Ingeominas, 2006; Montes et al., 2005. 2005 .
44
BOUNDARIES North: Romeral fault system (R.F.S) West: Romeral fault system (R.F (R.F.S.) .S.) South and Southeast: Central Cordillera(CC) and Serranía de San Lucas (SL) Pre-Cretaceous rocks East: Bucaramanga-Santa Marta fault system (B.S.M.F (B.S.M.F.).)
Figure 18. Lower Magdalena Valley Basin (15), location and boundaries.
Middle Magdalena Valley Basin (MMVB)
The MMVB correspond to what Kingston et al., 1983 called a poly-historic basin. Structural development took place through different stages linked to the t he tectonic events of the northwest corner of the t he South America that happened during Late Triassic, Middle Cretaceous, Early Paleogene and Middle Neogene. The basin stretch along the middle reaches of the Magdalena river and is bounded to the north and south by the Espíritu Santo fault system and the Girardot foldbelt, respectivel. To To the northeast the basin is limited by the Bucaramanga-Santa Marta fault system and to the southeast by the Bituima and La Salina fault systems (Llinas, J.C., 2001, La luna Oil, Internal Report). The western limit is marked by the westernmost onlap of the Neogene basin ll into the Serranía de San Lucas and the Central Cordillera basement (gure 19). General information: Gomez, et al., 2005; Gomez, et al., 2003; Rolón and Toro, Toro, 2003; Rolón, et al. 2001; Restrepo-Pace, 1999; Schamel, 1991; Barrero and Vesga, 1976; Feininger et al., 1970.
45
BOUNDARIES Southeast: Bituima and La Salina fault systems (B.S.F (B.S.F.S.) .S.) North: Espiritú Santo fault system s ystem (E.S.F.S) West: Onlap of Neogene sediments over the Serranía de San Lucas (SL) and Central Cordillera (CC) basement South: Girardot fold beld (GFB) Northeast: Bucaramanga-Santa Marta fault system (B.S.M.F.)
Figure 19. Middle Magdalena Valley Basin (16), location and boundaries.
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
Sinú-San Jacinto Basin/ foldbelt
The Sinú-San Jacinto Basin is located in northern Colombian, and it is the most prolic area in oil and gas seeps among Colombian basins. This under-explored basin limits to the east with the Romeral fault system; to north-northwest with the present Caribbean coast; to the west with the Uramita fault system, and to the south with the cretaceous sedimentary and volcanic rocks of the Western Cordillera (gure 20). The structural development of the basin is linked to the transpressional deformation generated by displacement of the Caribbean Plate. The Sinú portion of the basin is very ver y rich ri ch in mud diapirs and oil seeps. General information : Amaral et al., 2003; Duque-Caro, 1984; Mann, 1999; Ruiz et al., 2000; Villamil et al., 1999.
46
BOUNDARIES North- northwest: Present Caribbean coast West: Uramita fault system (U.F.S.) South: Cretaceous rocks of the Western Western Cordillera (WC) (WC ) East: Romeral fault system (R.F.S.)
Figure 20. Sinú –San Jacinto Basin (17), location and boundaries.
Sinú Offshore Basin Sinú Offshore Basin/foldbelt
This basin is entirely under Caribbean Cari bbean Sea waters and its structuring str ucturing consists of a number of northwest verging contractional fault-related folds and associated mud-diapirs. Its northeast limit is the Oca fault; the line separating the frontal thrust from non-deformed Caribbean crust sediments mark its northwestern limit (named South Caribbean Deformed Belt deformation front; gure 21); the southwest boundary is the offshore east boundary of the Urabá Basin and, the southeastern limit the present day shoreline (gure 20). This new limits denition includes the so-called “Sinú Marino” of former basins map of the ANH (gure 3). General information: Duque-Caro, 1984; Amaral et al., 2003; Ruiz et al., 2000; Villamil et al., 1999.
47
BOUNDARIES Northeast: Oca fault (O.F.) Southeast: Present day shoreline Northwest: South Caribbean Deformed Belt deformation front (S.C.D.B) Southwest: Uramita fault system (U.F.S) (U.F.S)
Figure 21. Sinú Offshore Basin (18), location and boundaries.
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
Tumaco Basin Tumaco Basin
The onshore onshore Tumaco Basin lies in the southwestern region of Colombia. Colombia. The basin basin limit to the north with the Garrapatas Garr apatas fault system; to the south it extend as far as the Colombian-Ecuadorian border; the eastern limit goes along the Cretaceous rocks of the Western Cordillera, and the west limit is the present day coastline of the Pacic ocean (gure 22). A Late Cretaceous-Neogene sequence shows gentle folding on top of a basaltic basement. Mud-cored anticlines are common. General information: Cediel et al., 1998; IGAC-Ingeominas, 2001.
BOUNDARIES 48
North: Garrapatas fault zone (G.F.Z.) (G.F.Z.) South: Colombian-Ecuadorian border East: Western Cordillera (WC) Volcanic rocks West: Coast line of the Pacic Ocean
Figure 22. Tumaco Basin (19), location and boundaries.
Tumaco Offshore Basin Tumaco Tumac o Offshore Basin
The Tuma Tumaco co Offshore Basin is located in the southwest marine region of Colombia, under waters of the Pacic Ocean. The tectonic setting of this basin is the forearc of the Upper Cretaceous subduction complex. The limits of this basin are: to the north the Garrapatas fault system; to the south the Ecuadorian border; to the east the present day shoreline, and to the west the inner trench wall of the present subduction zone (gure 23). The basin has a belt of mud-diapirs extending parallel to the shoreline. General information: Cediel et al., 1998; IGACIngeominas, 2001.
BOUNDARIES 49
North: Garrapatas fault zone (G.F.Z.) (G.F.Z.) South: Colombian-Ecuadorian border East: Present shoreline West: Trench of the Colombian Pacic subduction zone (C.P.S.Z.)
Figure 23. Tumaco Offshore Basin (20), location and boundaries.
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
Upper Magdalena Valley Upper Magdalena Valley (UMVB)
The UMVB is an intermontane basin located in the upper reaches of the Magdalena river. It is bounded to the east and west mainly by the pre-cretaceous pre- cretaceous rocks of the Eastern Cordillera and Central Cordillera, respectively, and by the Algeciras-Garzón strike-slip fault system and the Eastern Cordillera foothills thrust system to the southeast. The Bituima and La Salina fault fault systems and the Girardot foldbelt correspond to its northeastern and northern limits (gure 24). A basement-cored high, called the Natagaima-El pata high, divides the UMVB into two sub-basins: Girardot and Neiva. General information: Buttler and Schamel, 1998; Jaimes and De Freitas, 2006; Montes, 2001; Radic and Jordan, 2004; Ramón R amón and Rosero, 2006. Caribbean ar i bbeanSSea ea
. S . F . S . B
n a e c O c i f i c a P
PANAMA VENEZUELA
Pacific Ocean acificOcean COLOMBIA
Bogotá ogotá GF B IIbague 21
BRASIL
ECUADOR CUADOR
Neiva
CC
PERU
S . F . G . A
BOUNDARIES North: Girardot fold belt (GFB) 50
Southeast: Partially the Algeciras-Garzón fault system (A.G.F.S.)
ECUADOR
Northeast: The Bituima-La Salina fault system (B.S.F.S.) West: Pre-cretaceous rocks of the Central Cordillera (CC) NEIVA NEIV A SUB-BASIN
NW CENTRAL CORDILLERA 4000 3000 2000
T L U A F A N E L A D G A M
O C N A L B O D T L A L U A A S F
A T A T L L U P A A L F
1000
Ktg
GUACACALLO HIGH MAGDALENA RIVER
SE
T L U A F O T N I C A J N A S
GALLARDO HIGH
T L U A F O D E V E C A
GARZON MASSIF T L U A F A Z A U S
Kv
0 -1000 -2000
Taken from Fabre, 1995 Precambria iann
Color code according to the commission for the Geological Map of the World (2005)
Jurassic
Cretaceous
Pale Pa leog ogen enee
Neog Ne ogen enee
SW
NE
GIRARDOT SUB-BASIN 2000 m 1000 m 0 -1000 m -2000 m
Taken from Montes, 2001 Metamorphics Pale Pa leog ogen enee
Color code according to the commission for the Geological Map of the World (2005)
Paleozoic
Triasic-Jurassic
Lower Low er Cre Cretac taceou eouss
Upper Upp er Cre Cretace taceous ous
Neog Ne ogen enee
Figure 24. Upper Magdalena Valley Basin (21), location and boundaries.
Urabá Basin Urabá Basin
The Urabá Basin is a rectangular collision-related basin bounded bounded to the east and west by the strike-slip Uramita fault and the Serranía Ser ranía del Darien, respectively, and by the Murindó fault, the Mandé batholith and the Cretaceous rocks of the Western Cordillera to the south-southwest (gure 25). The northern-northwest extension goes as far as the Colombian-Panamá border in the North Panama Deformed Belt. The new boundaries are intended to include both the onland “Urabá” “Urabá” basin and “Urabá Marino” of the former ANH basin map. General information: Geotec, 1988; Ingeominas, 2006; Cediel et al., 1998. 79°
78°
77°
75°
76°
a rib rib b e an an S ea Caribbean Sea
Caribbean aribbeanSea Sea
10° P N
10°
N
M VENEZUEL
P D
Pacific acificOcean Ocean
9°
COLOMBIA OLOM I
9°
PANAMA SD
R
ECU DOR
ZIL
UU
. F
. S
8°
PERU
M
22
a cif cif ic ic Ocean Oce a n Pacific
BOUNDARIES
7°
7°
WC
North-Northwest: Colombian-Panamá Boundary Southwest: Mandé batholith (M.B.) and Murindó fault
South: Cretaceous rocks of the Western Cordillera (WC (WC))
51
M B
Medellin
6°
6°
East: Uramita fault system (U.F.S.) (U.F.S.) West: Serranía del Darien (SD)
8°
79°
78°
77°
75°
76°
N.P.D.B. N.P .D.B. North Panama Deformed Belt
SCHEMATIC SCHEMA TIC CROSS SECTION 3°
URABÁ BASIN
SW
Inversion
Transtension
NE
Sea level
Time sec 0
1
2
3
4
Color code according to the commission for the Geological Map of the World (2005)
Oceanic Crust
Paleogene
Neogene Figure 25. Urabá Basin (22), location and boundaries.
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
Vaupés – Amazonas Basin Vaupés – Amazonas Basin
This new proposed basin is a south-east plunging depression located in southeastern Colombia and bounded to the west and northeast by the Serranía de Chiribiquete and La Trampa-La Trampa-La Mesa de Carurú, respectively, and by the Vaupés arc to the north which is conformed by Lower Paleozoic Paleozoic rocks, forming structural highs. To To the north nor th of Mitú, an isolated area covered by Neogene sediments was included in this basin (gure 26). The south-southeastern extension of this basin reaches the Peruvian and Brazilian frontiers and may extend far southward as to join the Solimoes Basin. Basin.
52
BOUNDARIES North: Vaupés arc (VA) South-Southeast: Peruvian and Brazilian frontiers West: Basement high. Serranía de Chiribiquete (SC) East: La Trampa - Carurú highs (TC)
Figure 26. Vaupés – Amazonas Basin (23), location and boundaries.
Petro eol P Cetroleum olombianGeology Basins of
Colo Darío Barrero1 Juan Fernando Martínez1 Carlos A. Vargas2,3 Andrés Pardo2,4
B & M Exploration Ltda, Bogotá. Agencia Nacional de Hidrocarburos (ANH). 3 Universidad Nacional de Colombia, Departamento de Geociencias, Bogotá. 4 Universidad de Caldas, Departamento de Ciencias Geológicas, Manizales 1 2
Basin
leum gy of gy of bian
3.1 Caguán - Putumayo Basin Basin type
Foreland
Oil eld discoveries
19
Discovered oil reserves
365 MMBO
Recovered gas reserves
305 GCF
Overview
The Caguán-Putumayo Basin is the northern nor thern extension of the Oriente Or iente Basin of Ecuador.. This basin has an extension Ecuador ex tension of about 104.000 km2, and reserves of more than 365 MMBO have been found to date in 19 oil elds. Exploration in the basin was started by Texaco in 1948. In 1963 this company c ompany discovered discovered the major Orito oil eld with reserves in the order of 250 MMBO. The existence of a petroliferous system at work is documented by the several oil elds discovered in the basin. Two main structural plays: 1) high-angle reverse fault and, 2) wrench related anticlines account for most of the oil discovered so far. In addition, stratigraphic plays are also important exploration targets. Petroleum Geology (Figure 27) •
Hydrocarbon Evidence
Signicant production, one major oil eld (Orito), 18 minor oil elds and the presence of giant oil elds in the nearby Oriente basin in Ecuador are the evidence of the exploration potential of this basin. Giant Oil-seeps are active in the northern Caguán area. •
Source
Cretaceous limestones and shales from the Villeta Formation, with marine organic matter type II, high petroliferous potential and average TOC of 0.5-1.0 percent represent the best source rocks in the basin. Cretaceous organic shales from the Caballos Formation Formation,, with average TOC of more than 0.5% and organic matter type III, is a secondary source of hydrocarbons. •
Migration
Two pods of active source rocks within the Cretaceous sequence, located in the westernBasin. ank Migration of the basin, contributed the hydrocarbon charge the Putumayo pathways showtoseveral options. The mostinlikely migration route seems to be west to east along sandstones of the Caballos and
57
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
Villeta formations. Vertical migration along fractures and fault zones has also been documented. Expulsion of hydrocarbon started by Late Miocene soon after the formation of the major structures.
Caguán - Putumayo Basin
58
Figure 27. Caguán – Putumayo Petroleum system chart.
•
Reservoir
Cretaceous sandstones of the Caballos Formation is the main reservoir in the basin with an average thickness of 300 ft depending on paleorelief. Porosities range from 10% to 16% and permeabilities average 50 md. Secondary reservoirs are found in sandstones of the Villeta Formation and Pepino conglomerates. •
Seal
Cretaceous plastic shales of the Villeta Formation are excellent top and lateral seal units. Rumiyaco and Orteguaza shales are also potential seals. •
Trap
The main targets are structural traps associated with thrusts and sub-thrusts in the western side of the basin, and up-thrusts in the foreland basin. Additional traps are: pinch-outs, incised valleys, and carbonate buildups. •
Prospectivity
Oil elds in the basin are related to structural traps, mainly contractional faultrelated folds, and reverse faulting. Additional oil reserves could be found in signicant quantities trapped in sub-basement traps, wrench related anticlines, and drapes over basement highs and subtle stratigraphic traps at the eastern ank of the basin. Presence of these traps suggests that large part of the basin still has signicant exploration potential. 59
3.2 Catatumbo Basin Basin type
Foreland
Area
7,350 km2 / 1,800,000 acres
Wildcat wells
39
Oil eld discoveries
11
Overview
The Catatumbo Basin in Colombia is a southwest extension of the Maracaibo Basin. To date, eleven oil and gas elds have been discovered in this basin. Oil, reservoired in Cenozoic and Cretaceous sandstones and limestones, is trapped in faulted anticlines. The Cretaceous and Cenozoic in this basin represent two distinct tectonic and sedimentary settings. Cretaceous rocks are marine sandstones, shales and limestone that represent deposition in a broad shallow sea that extended across northern Venezuela and continued south through Colombia. Cenozoic rocks are uvial-deltaic shales and sandstones that were deposited in a foreland basin. Overall, reservoir porosity is best developed in Paleogene sandstones. Traps are wrench controlled, faulted anticlines that resulted from strike-slip convergence. Oil was sourced from the upper Cretaceous La Luna Formation and the lower Cretaceous Uribante Group. Oil generation began in the Late Eocene and continues through today. Seventy percent of the reserves were discovered between 1920 and 1950 and were based on surface exploration (mapping of surface anticlines.).
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
Most of the remaining hydrocarbon potential in this basin occurs in en-echelon folds associated with the regional left-lateral Chinácota fault system on the western ank of the basin, referred to as the “Catatumbo Flexure”in the northern nor thern portion of the basin (gure 8).
Catatumbo Basin
60
Figure 28. Catatumbo Petroleum system chart.
Petroleum Geology (Figure 28) •
Source
Cretaceous-pelitic rocks (La Luna, Capacho, Tibú and Mercedes formations) are widely present throughout the Catatumbo Basin; they are regionally distributed in the Maracaibo Basin and are considered one of the richest hydrocarbon sources in the world. The La Luna Formation is the principal source in the basin and is 200 ft. thick. The TOC ranges between 1.5% to 9.6%, with average 3.8%. The La Luna Luna Formation is currently in the oil window. window. •
Migration
Three distinct migration systems have likely operated to ll the Catatumbo sub-basin traps that were developed in the late Miocene-Pliocene. The lithological character of the Cretaceous sequence, very ne grained sands and homogeneous limestone and shale, favored the development of in-situ oil reservoirs with very little or no hydrocarbon migration. Lateral migration along sandstone bodies and vertical migration along fractures are the two most effective migration pathways. •
Reservoir
Main reservoir rocks are Cretaceous shallow water limestones and Cretaceous sandstones (Uribante Group, Capacho and La Luna formations). Deltaic sandstones of Paleogene age (Catatumbo, Barco, Mirador and Carbonera formations) are also good reservoirs. Additionally, fractured basement rocks are also considered to be potential reservoirs. •
Seal
Thick marine and non-marine shales in the Cretaceous and Cenozoic Cenozoic sequences form potential seals. •
Trap
The Catatumbo Basin shows a wide variety of traps: t raps: normal faults with partial inversion, subthrust structures, triangular zones and structures associated to inversion systems are important structural traps. Some oil entrapments within the Paleocene, Barco and Catatumbo formations are considered as indigenous or in-situ. The entrapment and production of Cretaceous oil is basically controlled and associated with the secondary porosity developed by fracturing of the same Cretaceous rock. •
Prospectivity
The Catatumbo Basin has been one of the most prolic basins in the country. Commercial hydrocarbon production comes from structures related to asymmetric folds affected by inversion. The western zone of the basin is a fold belt and recent studies in the area indicate potential exploration plays along thrust zones. The main oilelds in the basin are the Rio de Oro, Tibú - Socuavo, Carbonera, Sardinata, Rio Zulia, Petrolea and Puerto Barco. The Catatumbo Basin is a moderately explored basin which has produced more than 450 MMbbl of oil and 500 Gcfg since 1920.
61
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
3.3 Cauca-Patía Basin Basin type
Collision Related
Area
12,800 km2 / 3,200,000 acres
Wildcat wells
5
Seismic coverage
1,000 km
Source Rocks
Chimborazo and Nogales shales
Reservoir Rocks
Chimborazo and Chapungo sandstones
Seal Rocks
Guachinte - Ferreira shales
Overview
The Cauca-Patía Basin lies between the Central Cordillera to the east and the Western Cordillera to the west. The basin is mapped as an elongated geomorphic depression that extends for about 450 km north-south nor th-south and averages 40 km eastwest (gure 9). The basin was developed by collision of an intra-oceanic island arc against the irregular continental margin of the northwestern part of South America. Age relationships of molasse deposits that were folded and thrusted show that diachronous wasevidence completed frompresence south toof north during late Cretaceous to Neogene.collision The best of the a hydrocarbon system is the Matacea Creek oil seep. Petroleum Geology (Figure 29) 62
•
Hydrocarbon Evidence
Presence of a hydrocarbon system at work is given by the oil and gas shows reported in a few wells drilled in the Cauca Valley area, and by the Matacea Creek oil seep in the Patía region. •
Source
Geochemical analyses carried out on 60 samples from 6 surface sections and one oil sample from the Matacea Creek oil seep indicate that the shaly Nogales Formation of Late Cretaceous age and the Eocene Chimborazo Formation have the highest source potential. TOC contents are greater than 2 % for Cretaceous rocks and between 1 and 2 % for the Eocene shales. Organic matter consists of a mixture of kerogene type II and IIl. In the Patía region the Chapungo Formation Formation is considered a potential source rock. •
Migration
Migration of hydrocarbon occurred along sandstone beds of Paleogene age and fractures related to fault zones. Migration started in the Late Miocene and continues to date as demonstrated by the occurrence of fresh hydrocarbons found in the Matacea Creek oil seep. •
Reservoir
Several intervals with reservoir characteristics are present throughout the sedimentary sequence of the basin. The main siliciclastic reservoir is the Chimborazo Formation which has porosities of 5 -15 % and average permeabilities of 100 md.
•
Seal
Cauca-Patía Basin
Top and lateral seals are provided by claystones and shales of the Chimborazo, Top Guachinte and- Ferreira formations. Nevertheless, seal is the main risk factor in the basin. •
Trap
More than 1,000 km of seismic reection proles across the basin show the presence of high-side and subthrust anticlines. In the Cauca Valley area imbricate thrust systems provide the main structural traps. Stratigraphic pinch-outs and onlaps are also potential targets.
STRATIGRAPHIC UNIT
Molasse
Mosquera/Guachinte Collision related oceanic basin
P. Morada/Chimborazo
First oblique collision
Río Guabas/Agua Clara, Chapungo/ Nogales Remnant oceanic basin
Diabasico/Amaime
Ridge and plateau basalts
Figure 29. Cauca – Patía Petroleum system chart.
63
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
•
Prospectivity
Structures characterized by large anticline and fault-related traps in the Patía region together with the existence of a proven petroleum system provide attractive targets to explore for liquid hydrocarbon.
3.4 Cesar- Ranchería Basin Basin type
Intramountain
Area
11,630 km2 / 2,900,000 acres
Wildcat wells
14
Overview
The Cesar- Rancherí Rancheríaa Basin in the northeas northeastt part of Colombia covers an area of 11,630 km2. Hydrocarbon exploration began in the basin with the well El Paso-1 drilled by the Tropical Oil Company. This limited area is relatively underexplored and contains only 14 wells, most of which were drilled before 1955. High hydrocarbon potential may exist in the relatively unknown subthrust region anking the Perijá Andes. Two structural plays have been mapped in this area: 1) Cretaceous fractured limestones, 2) Cretaceous and Paleocene sandstoness in structural traps. sandstone 64
Petroleum Geology(Figure 30) •
Hydrocarbon Evidence
Marginal gas production in the Compae eld, and oil shows reported at a number of wells provide clear evidence of a working hydrocarbon system. API gravity ranges from 24º to 37º. •
Source
Molino, La Luna, Lagunitas and Aguas Blancas formations show organic richness, quality and maturity that indicate they are effective source rocks. Kerogen type is ll / Ill. Average TOC for the formations are: Molino Fm. 1.0; La Luna Fm. 1.4 and Aguas Blancas Fm. 1.39. •
Migration
Secondary migration seems occur during transpressional events that began in Eocene time and lasted until today. Migration pathways are wide fracture systems associated to fault zones. •
Reservoir
The main reservoirs are the Lagunitas Lagunitas and Aguas Blancas Blancas fossiliferous fossiliferous limestones limestones associated with carbonate ramps. The average gross thickness reported in wells is 500 ft with standard porosity around 5%.
•
Seal
Cretaceous and Cenozoic plastic shales are the main top and lateral seal rocks in the basin.
Cesar Ranchería Ranchería Basin •
Trap
Structural traps associated with subthrust closures in the Perijá region, wrench anticlines in the central region, and ower structures associated to the Oca fault system in the north area, are the most prospective targets. •
Prospectivity
In the basin it is possible to identify three main play types: 1. Upper Cretaceous, Aguas Blancas/Lagunitas limestones in subthrust anticline closures. 2. Paleogene/Neogene, Cerrejón and Tabaco sandstones in anticline closures associated to Oca and El Tigre transcurrent tr anscurrent faults. 3. Upper Cretaceous, Lagunitas fractured limestones associated to Oca and El Tigre transcurrent faults. faults.
65
Figure 30. Cesar – Ranchería Petroleum system chart.
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
3.5 Chocó Basin type
Fore-Arc?
Source rock
Iró Shale
Reservoir rocks
Iró and Mojarra sandstones
Seal rocks
La Sierra and Itsmina claystones
Wildcats Wells
5
Overview
The Chocó Ch ocó Basin Ba sin covers co vers about a bout 42,000 4 2,000 km2. To date 5 wells have been be en drille dr illed, d, with coverage of 7,000 km2 / well, a density much less than other basins in Colombia. Surface indications for oil and gas have been reported in numerous locations. Subsurface shows of oil and gas were encountered in the Buchadó-1, and Majagua-1 wells. Petroleum Geology •
Source
All the hydrocarbon shows found in the Chocó Basin are believed to have been generated primarily from the Iró Formation (geochemical analyses). 66
The To Total tal Organic Carbon (TOC) content of the Iró Formation (condensed sections, cherts and shales) has ranks from fair to good. •
Migration
Any oil generated must have migrated laterally up dip to the anks of structures. Long distance lateral migration of hydrocarbons is suggested on the basis of geochemical, stratigraphic and structural data. Vertical migration pathways are associated with fault systems. The critical migration period occurred after deposition of the sealing units about 5 Ma, and continues to date. •
Reservoir
Carbonate and siliciclastic rocks from the Iró and the Mojarra formations (Middle Miocene) are the major potential reservoir rocks. Naturally fractured cherts are abundant in the basin and are related to faulting. •
Seal
Sealing rocks occur throughout the sedimentary column, represented by clay units. These units are homogeneous, laterally continuous, with excellent ductile properties. The La Sierra (Oligocene) and Itsmina (Lower Miocene) formations are the regional seals. •
Trap
Several basement structural highs, mud-cored anticlines, diapir anks, thrust anticlines, normal fault roll-overs, stratigraphic geometries, and highly fractured carbonates and cherts along fault zones are all potential traps.
•
Prospectivity
Geochemical data indicate the existence of the Iro-Mojarra (?) petroleum system. TOC content, kerogene type II and III, and Hydrogen Index indicate a good oil prone source rock. Oil generated may have migrated and been trapped in large mud-cored anticlines, roll-overs associated with listric normal faults and large high-side closures in fault propagation folds.
3.6 Eastern Cordiller Cordillera a Basin type
Inverted Graben / Fold belt
Area
60,000 km2 / 14,800,000 acres
Field discovered
10 (8 oil elds - 2 gas eld)
Wildcat wells
38
Discovered Oil
1,700 MMBO
Overview
The Eastern Cordillera Fold Fold Belt covers an area of about about 60,000 km2. It is located between the Magdalena River Valley and the Llanos Cenozoic Foreland Basin. In the present work, the previous boundaries have been slightly modied to include in both sides, the frontal thrust of the fold belt. Therefore, the so called eastern and western foothills which contain the giant Cusiana and the major Provincia oil elds located in the hangingwall of the frontal thrusts, are considered here as a part of the Eastern Cordillera basin. The beginning of the exploratory process in the basin was oriented to conrm accumulation in anticline structures located in the surrounding areas of Tunja, where multiple oil seeps were found. During the last three decades, drilling has been mainly oriented to the exploration of structural traps on the foothills. During the Triassic-Jurassic Triassic-Jurassic and late Cretaceous, tensional/transtensional tensional/transtensional stresses, produced a system of asymmetric half-graben basins lled continuously with alternate marine and near shore to continental deposits. The deformation of these deposits occurred as a succession of events. The rst event of late EoceneEarly Oligocene age generated an imbricated system. The imbricated system was eroded and covered by upper Oligocene deposits. A subsequent transpressional event during Miocene to Pleistocene reactivated pre-existing thrust faults and re-folded the structures concomitant with the uplift of the t he Cordillera. Petroleum Geology (Figure 31) •
Hydrocarbon Evidence
Five decades of exploration history in the basin has lead to the discovery of about 1,700 MBO, 2.0 TCFG and a total of 10 elds, including the giant Cusiana and Cupiagua elds, and the large gas-condensate Gibraltar discovery.
67
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
•
Source
Eastern Cordillera
Two condensed sections of Mid- Albian and Turon Turonian ian age, deposited during worldwide anoxic events, are considered the main source. In addition, less important source rocks are believed to be present in the lower and upper Cretaceous. Main hydrocarbon generating sources contain T.O.C. T.O.C. values between 1.0 and 3.0 % and kerogen types I and II. •
Migration
The rst generation pulse occurred during during the Late Cretaceous, but most most of the petroleum generated seems to be lost because of the lack of traps at that time. A second pulse occurred from the Miocene to recent times, and it is responsible for lling the giant traps in both foothills.
68
Figure 31. Eastern Cordillera Basin Petroleu Petroleum m system chart.
•
Reservoir
The most important i mportant petroleum reservoi reservoirr rocks roc ks were deposited during Albian and Cenomanian time and Paleogene siliciclastic units with a wide range of petrophysical petrophys ical properties: average porosities between 5-10 % and permeabilities in the order of 4-100 md. •
Seal
The seals for the Paleogen Paleogenee sandstone reservoirs consist of interbedded shales. The regional seal for for the Cretaceous reservoirs are thick shales of marine origin. origin. •
Trap
The main structural structural features are basement involved involved reverse faults, faults, resulting from the inversion of pre-existing normal faults, contractional fault-related folds and duplex structures. •
Prospectivity
The Neogene deformation of sediments in the basin was probably related to strike-slip motions. It is most likely that future discoveries will be associated with traps formed by transpression. Fault-bend propagation folds and triangle zones are the main objectives in the folds, Easternfault Cordillera. A potential play in the axial zone is related to accumulation against salt domes, and nonconventional gas plays associated to coal beds. 69
3.7 Eastern Llanos Basin type
Cenozoic Foreland
2D seismic shot
> 96,000 km
Wildcat wells
260
Number of discoveries
68 oil eld, 2 giant, 1 major eld
Overview
The Eastern Llanos Basin is located in the Eastern region of Colombia. Geomorphologic boundaries are the Colombian-Venezuela border to the north, Macarena high and Vaupés Arch to the south, Guaicaramo fault system to the west, and Guyana Shield to the east. (gure 14) The evolution evolution of the basin started in the Paleozoic with a rifting phase. Siliciclastic sediments were deposited over the crystalline Precambrian basement, from Triassic to Late Cretaceous the basin was the eastern shoulder of a major rift system. Since the Maastrichtian to Paleocene, this basin became a foreland. From Miocene to recent times the basin has been repository of thick molasse deposits. Cretaceous source rocks range from immature to marginal mature within the region to the east of the frontal thrust. Main reservoirs are siliciclastic units of Late Cretaceous and Paleogene age. Analysis of the individual components
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
of the migration systems within the basin is complicated by thinning of the stratigraphic section; and the development of more sand-prone facies towards the Guyana Shield.
Eastern Llanos
70
Figure 32. Eastern Llanos Basin Petroleum system chart.
Petroleum Geology (Figure 32) •
Hydrocarbon Evidence
More than 1,500 1 ,500 MMBO of recoverabl re coverablee oil is offi ciall ciallyy documented. Two giants, (Caño-Limón and Castilla) three major (Rubiales, Apiay and Tame Tame Complex), and more than fty minor elds have been discovered. •
Source
Source rocks for the Llanos Foreland Basin are in fact located beneath the east ank of the Eastern Cordillera. Mixed marine-continental shales of the Gachetá Formation with kerogen type II and III, TOC ranging from 1-3% and 150-300 ft of effective thickness are the main source. •
Migration
Two pulses of migration migration have have been documented. documented. The rst one during the Upper Upper Eocene-Oligocene. The second pulse of migration started in Miocene time and is continuing at the present. •
Reservoir
The Paleogene Carbonera (C-3, C-5, and C-7) and Mirador sandstones are excellent reservoir units. Within the Cretaceous sequence several sandstone intervals are also excellent reservoirs. Without exceptions, sedimentary thickness increases in an east to west direction. Porosity decreases in the same direction from 30% to near 10%. Pay thickness varies from a few feet up to 180 feet, depending on the location of the well within the basin. API gravity ranges from 120 to 42º. •
Seal
The C-8 unit of the Carb Carbonera onera Formati Formation on has been tradi traditiona tionally lly consi considered dered as the regional seal of the basin, but because of its extension the best seal is the Carbonera C-2 Unit. The Carbonera even numbered units are recognized rec ognized as local seals as well as the Cretaceous Gachetá and Guadalupe formations that may be self-sealant. •
Trap
Exploration drilling has been concentrated in normal, up-to-the basin (antithetic) faults. Poorly tested reverse fault anticlines, low-relief anticlines and stratigraphic traps (pinchouts, paleohighs, channels, etc.) are all high potential exploration targets. •
Prospectivity
This basin has been moderately drilled and subtle stratigraphic traps have not been deeply studied. Potential areas for hydrocarbon accumulation are located in the southern and eastern portion of the basin where pinch-out of reservoirs are affected by meteoric water forming hydrodynamic traps. The southwestern part, south of the Castilla Field, is also a highly prospective area.
71
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
3.8 Guajira
Guajira
Basin type
Transtensional Transtensio nal
Area
12,600 km2 / 3,110,000 acres
Wildcat wells
18
Gas discoveries
Ballena (1.5 TCF) and Riohacha (86.5 GCF)
Overview
The Onshore Guajira Basin covers an area of 12,600 km2 and is located in the northernmost part of Colombia. The lower Guajira Basin is the result of a releasing step-over of Cuisa-Oca transcurrent fault systems, thus generating a transtensional margin basin. North of the Cuisa Fault, the upper Guajira is structurally related to rifting that occurred north of Maracaibo Lake. Exploratory drilling started with the Rancheria-1 well, spudded in 1948. To date, only 18 wildcats have been drilled with two gas elds discovered.
72
Figure 33. Guajira Basin Petroleum system chart.
There is a proven gas generation-migratio generation-migration n system within the basin. Migration is enhanced by structural geometry, which focuses migration paths from a thermogenic gas source sitting offshore. There are several documented developments of porous carbonate buildups on horst blocks. The two main plays are the Paleogen Paleogenee basal sandstone on basement with an onlap/pinchout component and the Miocene carbonate buildups. The Ballena and Riohacha elds are within this area and produce from the carbonate play. Petroleum Geology (Figure 33) •
Hydrocarbon evidence
It is proven by the two gas elds discovered in the basin. Turbiditic sandstones with average porosities of about 17 % are the main targets. t argets. •
Source
Cretaceous Colon, La Luna, Cogollo shales and the Neogene Castilletes Formation contain kerogen type II and are considered good oil source rocks. Organic matter of Paleogene-Neogene source rocks is strongly gas-prone. The Neogene Castilletes Formation has TOC values ranging from 1 5-2.0 % and kerogen type II and III. •
Migration
Most of the structures were formed during Late Paleogene-Early Neogene. Secondary migration of hydrocarbon most likely occurred soon after the rst phase of structur¬ing by Late Neogene. •
Reservoir
Siliciclastics and carbonates are important reservoirs in the basin. Neogene limestones of the Uitpa and Jimol formations have very good moldic porosity and net pay thickness up to 100 ft. In addition, fractured basement can also be considered as a potential reservoir reser voir (e.g. Venezuela, Venezuela, La Paz –Mara elds.) •
Seal
Top and lateral seals for Cretaceous reservoirs in the Guajira are adequate Top where Paleocene and lower Eocene shales are present. Base seal for PaleogeneNeogene reservoirs is variable. •
Trap
Several potential structural traps of Neogene age are the result of deformation generated by the Cuisa and Oca faults. Main stratigraphic traps are onlaps and truncations against basement highs. Carbonate mounds are very important trapping geometries. •
Prospectivity
The PGG-1 Well (Venezuela) drilled carbonates of the La Luna Formation saturated with oil, thus documenting the existence of a hydrocarbon system in the southeastern corner of the upper Guajira Basin. The generation pod is located to the east of the well in the Cosinetas Basin. Highly prospective structural traps exist in the western ank of the Cosinetas Basin in the upper Guajira. Structural
73
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
and stratigraphic traps in the lower Guajira have good exploration potential. Oligocene carbonates, fractured by the Oca Wrench System, are the main exploratory target. Proved Plays: Lower Miocene sandstones and limestones and middle Miocene turbidites. Unproved Wrench-Related structures Cuisa and Oca faults. Onlaps andPlays: truncations, imbricated thrust associated sheets andtoOligocene carbonate stratigraphic plays and fractured basement.
3.9 Guajira Offshore Basin Overview
The Guajira offshore offshore Basin is the northernmost sedimentary area of Colombia. It extends from the northernmost point of the Guajira Peninsula to the mount of the Magdalena River in the southwest. Shallow offshore is considered to have water depths from 0-600 feet. Source rock could be the Castilletes Formation deposited in the deeper and more subsident part of the basin. The main reservoir rocks are carbonates buildups, a Paleogene basal sandstone and submarine fan turbidites. Migration of hydrocarbon from the deep offshore is enhanced by the structural conguration.
74
Hydrocarbon accumulation has been proven in the shallow offshore (0’-600’) by production in the Chuchupa gas eld. In addition, westward of Santa Ana-1 well geochemical analyses on offshore piston cores, resulted in the identication of thermogenic gas and oil in such samples. At least three plays are present over the area. The giant Chuchupa gas eld produces from the basal sandstone play. The carbonate play is producing in the Ballena gas eld. The deep offshore greater than 600ft of water is very probable the area for the Miocene fan play. Petroleum Geology •
Source
Oil and gas was found in piston cores offshore Guajira (Texaco program 1999). The main source rock in the area area could could be the offshore extension of the Castilletes Formation deposited in the deeper and more subsident part of the basin. A Cretaceous or even a kimmerigdian source rock could be present, in the deep offshore area, north of the Cuisa Fault. •
Generation and Migration
Generation and migration of hydrocarbons is enhanced by structural conguration which focuses migration paths from an early thermogenic source in the deep offshore toward the Chuchupa, Ballena and Riohacha reservoirs. •
Reservoir
Two main reservoirs types have been documented in the area: 1) carbonate buildups, a reservoir type which produces gas in the Ballena and Riohacha elds and, 2) the siliciclastic reservoirs composed of the Paleogene basal sandstone,
producing in the Chuchupa gas eld, and the submarine fan sandstone which extends to the deep offshore. •
Seal
Seal in the basin is provided by thick sequences of Paleogene and Neogene shales. •
Trap
Structural and stratigraphic traps are abundant in the basin. Roll-overs produced by listric normal faults provide excellent large trapping structures. In addition, drapes over basement highs, carbonate buildups and pinchouts / onlaps are good combination traps. •
Prospectivity
The fact that large quantities of gas have been storaged in two t wo main types of plays (Ballena-Chuchupa-Riohacha) and large structures are present with an excellent operation conditions, together with a growing demand of gas in the nearby countries, are good reasons to rank this area as highly prospectivity.
3.10 Los Cayos Cayos Basin Basin type
Transpressional Transpressio nal
Area
73,500 km2 / 18,160,000 acres
Discovered oil reserves
None
Wildcat wells
none
Overview
Colombia has an area of 589,560 km2 in the Caribbean Sea. Los Cayos Basin covers an extension of approximately 73,500 km2. The San Andres and Providence archipelago, located 770 km northwest of the Colombian mainland is comprised of the islands of San Andres, Providence and Santa Catalina within the basin. Petroleum Geology •
Hydrocarbon evidence
This is given by oil shows shows in wells drilled in the nearby area, and and oil slicks related to basement highs. •
Source
Source rocks are not well documented, but the occurrence of oil shows is an evidence of their existence. •
Migration: Unknown.
•
Reservoir
Siliciclastic Eocene deposits and Miocene-Oligocene reefal limestone. Porosity for siliciclastic rocks could be around 25%, and, 10% for limestone. •
Seal
Reported Oligocene-Miocene shales are potential seals.
75
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
•
Play Trap
Structural domes and normal faults. Pinch-outs and carbonate build-ups are potential stratigraphic traps. •
Prospectivity
No commercial hydrocarbon discoveries have been reported up to date. However, oil shows indicate exploration potential. Structural and stratigraphic traps are identied in seismic proles.
3.11 Lower Magdalena Valley Basin type
Transtensional Transtensio nal
Area
41,600 km2 / 10,280,000 acres
Wildcat wells
117
Tested Test ed oil reserves (Dec/05)
71 MMbbl
Seismic
20,300 km
Well Coverage
145 km2 / well
Oil eld discoveries
17
Overview 76
The Lower Magdalena Basin is located in the northwest of Colombia where oblique subduction along the Romeral fault system has produced transpressional and transtensional deformation since late Cretaceous to present day. The Lower Magdalena Basin is limited to the northeast by the Bucaramanga - Santa Marta fault system; to the south by the Central Cordillera and to the west by the Romeral fault system (gure 34). This basin is subdivided by three structural elements that t hat have controlled sedimentation since Eocene to late Miocene. These structural elements are: The Plato sub-basin to the north, the Cicuco Arch in the central part, and the San Jorge sub-basin to the south. Petroleum Geology (Figure 34) •
Hydrocarbon Evidence
Abundant oil and gas seeps are evidence of the existence of a prolic Petroleum System at work. •
Source
Early Miocene shales (Lower Porquero Fm.) have been recognized as the main source of hydrocarbons in the basin. These shales are of great thickness, rich in organic matter and kerogene type II. The Cienága de Oro Formation has an upper interval with fair-to-rich content of organic matter, type - III, within the oil window in the deepest areas of the basin. This interval could be considered as deposited during a maximum ooding event. The available source rock data suggests a pod of active source rock; probably of Cretaceous age; coinciding with the areas of greater sediment depth.
Lower
•
Migration
Magdalena
Pods of active source rock in generation/expulsion phase are present in an extensive area in the so-called Plato sub-basin; between the wells Guamito-1 to the northeast and Pijiño-1 to the south. API gravity for oil generated within the basin varies between 30° to 52°. The sulfur content is very low; while the paraffin
Valley
77
Figure 34. Lower Magdalena Valley Basin Petroleu Petroleum m system char t.
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
concentration is relatively high. Various geochemical parameters indicate that the majority of oil originated in a relatively dioxic proximal siliciclastic environment. Four different migration pathways have been proposed: 1) The Cicuco-Boquete area. 2) Momposina area. 3) Guepaje area and 4) Apure-region. Migration most likely happens along network of fracture and fault planes. •
Reservoir
Oligocene sandstones and limestones (Cienaga de Oro Formation) are the main reservoirs in the basin. The gross thickness is 300 ft, with an average porosity of 15%. •
Seal
Shales of the upper Porquero and Cienaga de Oro formations deposited during a period of rapid subsidence, have excellent physical characteristics as a sealing unit. The deep-water shales are the regional top seal for the under-laying reservoir rocks. The younger Tubará Tubará Formation (Middle Miocene to Lower Pliocene) is also a sealing unit. •
78
Trap
Diverse structural trap types highlights the basin potential, among others: structural traps associated with high-side closures in contractional contract ional faults, anticline closures in the footwall of normal faults, structures related to ower geometries generated by transpression, roll-overs in the hanging-w hanging-wall all of listric listr ic normal faults, all of them are important structural exploration targets in the basin. Stratigraphic traps are also of great economic impact, since production from carbonates has long been established and submarine fan turbidites are also prospective. •
Prospectivity
Presence of oil elds and abundant oil seeps, together with a great variety of structural traps and recent generation from pods of active source rock in deep synclinal structures indicate very good potential for discovery of new reserves.
3.12 Middle Magdalena Valley Valley Basin type
Poly-historic, Poly-histo ric, Rift to Broken Foreland
Area
34,000 km2 / 7,900,000 acres
Wildcat wells
296
Oil eld discoveries
41
Discovered oil reserves
1,900 MMBO
Discovered gas reserves
2.5 GCF
Overview
The Middle Magdalena Basin is located along the central reaches of the Magdalena River Valley between the Central and Eastern Cordilleras of the Colombian Andes. The exploratory process has been oriented mainly towards the identication of structural traps in the Paleogene sequences. Stratigraphic subtle traps have not adequately been studied yet. The sedimentary record
shows a succession of Jurassic continental deposits overlaid by Cretaceous sediments, both calcareous and siliciclastics, are of transitional to marine origin. The Paleogene Paleogene sequence sequence is made up of siliciclastic rocks rocks deposited deposited mainly under continental condition with some marine inuence. Three major deformational phases are presents in the basin; rifting, thrusting and wrenching, responsible for all type of trap tr ap geometries.
Middle
Magdalena
Valley
79
Figure 35. Middle Magdalena Valley Basin Petroleum system chart.
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
Petroleum Geology (Figure 35) •
Hydrocarbon evidence
A century of exploration history in the basin has lead to the discovery of about 1,900 MMBO, 2.5 TCF and a total of 41 elds, including the rst giant in Colombia, La Cira-Infantas eld. •
Source
Cretaceous Limestones and shales of the La Luna and the Simiti-Tablazo formations are the main source rocks in the basin. TOC are high (1-6%) and organic matter is essential type II, Ro reach values of 0.6 -1.2 %. The main source rocks were deposited during two worldwide anoxic events. •
Migration
The Eocene unconformity separates the primary reservoir from the underlying active source rocks, forming an ideal a plumbing system for the migration of petroleum. Major migration pathways consist of: 1) Direct vertical migration where La Luna sub-crops the Eocene unconformity 2) Lateral migration along the Eocene sandstone carrier 3) Vertical migration via faults in areas where the La Luna does not sub-crop the Eocene unconformity. unconformity. Critical period occurs during the Upper Neogene, about 5 Ma. , and continue locally today. • 80
Reservoir
97% of the proven oil in the basin comes from continental Paleogene sandstones (Paleocene-Miocene), Lisama, Esmeraldas-La Paz, and ColoradoMugrosa formations, formations, with average porosities 15-20% and average permeabilities 20-600 md. Lightly explored reservoirs are fractured systems of the Cretaceous Limestones Basal Limestone Group and La Luna Formation. •
Seal
The seals for Paleogene sandstone reservoirs reservoirs consist of interbedded interbedded non marine ductile claystones, mainly from the Esmeraldas and Colorado formations. The seals for potential Cretaceous limestone reservoirs are marine shales of the Simiti and Umir formations. •
Trap
Exploration has been directed to prospecting accumulations in structural closures form by major asymmetric anticlines, among them: 1) Contractional fault-related folds hidden beneath surface thrust, 2) duplex structures with fault independent closure, 3) fault-dependent closures in which reservoir strata dip away from the fault, 4) very important; traps in the low side of sealing faults. •
Prospectivity
The Middle Magdalena Basin is one of the most explored basin of Colombia where 41 elds have been discovered discovered on Paleogene Paleogene deposits. Surprisingly it still contains one of the most prolic areas yet to be explored: the Cretaceous carbonate plays.
Potential exploration areas are mainly related to inverted normal faults and subthrust anticlines. Subtle stratigraphic traps associated with Miocene-Upper Miocene-Upper Eocene onlaps, incised channels and truncations are also major objectives for future exploration.
3.13 Sinú-San Jacinto Basin type
Accretionary Prism
Area
38,500 km2 9,500,000 acres
Discovered reserves
Marginal
Oil eld discoveries
Non commercial
Wildcat wells
44
Source rocks
Cansona Formation
Reservoir rocks
Paleogene sandstones
Seal rocks
Floresanto Formation
Overview
The Sinú - San San Jacinto Basin/foldbelt Basin/foldbelt was formed formed as an accretionary accretionary prism along the South American continental margin due to subduction of the Caribbean Plate. The San Jacinto Fold Belt was developed in the Eocene and consists mainly of sedimentary rocks and slivers of volcanic rocks scrapped off the Caribbean Plate. The Sinú belt is younger and consists mainly of sedimentary deposits along the northwestern margin of Colombia, incorporated later in the accretionary prism during the Miocene. Numerous oil and gas seeps are the evidence of a petroleum system at work. Clastic and carbonate potential reservoirs together with strong structuration indicate high prospectivity. The enormous amount of oil seeps are evidence of hydrocarbon generation. Good siliciclastic reservoirs are present throughout the area sealed by the Floresanto shaly facies. Petroleum Geology (Figure 36) •
Source
Hydrocarbon generation began in the Miocene, but some earlier generation could have occurred in the Cretaceous (Cansona Formation). The enormous amount of oil seeps are evidence of hydrocarbon generation in the region. The Cansona Formation is favorable for the generation of liquid hydrocarbons and consists mainly of organic rich kerogen types I-II. The Porquero and Floresanto formations and the muddy facies of the Cienaga de Oro Formation frequently show a gas prone signature with type II, III kerogen. •
Migration
Migration of hydrocarbon along fractures is documented by the abundant oil and gas seeps.
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Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
•
Reservoir
Sinú-San Jacinto
The main potential reservoirs are siliciclastics deposited during the Eocene Miocene. These deposits vary from continental to uvial-deltaic to marine and also include shallow water carbonate car bonate deposits.
82
Figure 36. Sinú – San Jacinto Basin Petroleum system chart.
•
Seal
Overlapping sealing units are present in the entire basin. The seals are associated with translapping or migration of facies changes from marine to continental environments. •
Trap
It is possible to identify different kind of plays with good exploratory potential; structural traps in thrust-related closures and stratigraphic traps present at the northern and of the San Jacinto fold belt. Shale-diapirs anks could also be exploration targets. •
Prospectivity
Abundant oil and gas shows, clastic and carbonate potential reservoirs, reser voirs, together with strong structuration indicate high prospectivity.
3.14 Sinú Offshore Basin type
Accretionary Prism
Discovered reserves
None
Wildcat wells Basin Overview
The Sinú Offshore area lies in the coastal waters of northwest Colombia. It extends from the mouth of the Magdalena River in the northeast to the northern end of the Urabá Gulf in the southwest. Water depth over almost all of the area is less than 1.200 meters. Approximately, two thirds of the area is shoreward of shelf break that roughly parallels the coast. The remaining third consists of shallow water with depth on the range from zero to ca. 200 20 0 meters. The Sinú Offshore is juxtaposed to the west margin of the Sinú-San Jacinto Basin/Foldbelt (onshore) a structurally prospective area that include at least two genetically distinct packages of sedimentary rocks Petroleum Geology •
Source
The principal likely source for thermogenic hydrocarbons in the Sinú Offshore domain are Cenozoic marine condensed sections and prodelta shales. In addition, there are strong evidences in the adjacent onshore area for the presence of an Upper Cretaceous source that could have a lateral equivalent in the offshore area. This statement is supported by geochemical analyses done in onshore oil seeps that relate then to the t he Cretaceous La Luna source rock. •
Generation and Migration
Active generation and migration is based on the occurrence of: 1) Numerous shows of gas in nearly all of the offshore wells. 2) Several owing oil and thermogenic gas in the nearby onshore area. 3) Traces of oil found in the San Bernardo-IX well. 4) Evidence of thermogenic hydrocarbons in extracts from
83
Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
nine piston core samples, collected by British Petroleum. 5) The existence of a Cretaceous oil prone generative system remains hypothetical •
Reservoir
The basin contains sandstones that are potential reservoirs. Presence of negrained sandstone has been documented by several wells drilled in the area. A few wells have reported the existence of segments composed of coarse grained sandstone. Large accumulation of sandstone turbidites are expected against the anks of shale diapirs. •
Seal
Sealing units occurs throughout the basin and they consist of shales deposited in prodelta environments. The ank of diapirs could act as good lateral seal. However, the seal prospect effi ciency appears to be a critical cr itical point for the t he prospectivity in this area. •
84
Trap
The size of the traps is large and most of them lie at a depth of 1 to 2.5 seconds two-way-time on seismic. Thrust-related anticline traps with primary objectives of Oligocene low-stand sandstone are the main targets. In addition, several large combination traps formed by sin-tectonic onlaps of Miocene sandstone, structural traps on the anks of shale piercement-diapirs, low-side roll-overs of Pliocene sandstone involved in listric normal faults and pure stratigraphic traps, form the bulk of exploration opportunities in the area. •
Prospectivity
The area covering the Sinú Offshore O ffshore domain is prospective because there are numerous structural and stratigraphic plays. These plays are supported by adequate source rock, siliciclastic reservoirs and active ac tive generation and migration of hydrocarbons. The presence of large quantities of liquid hydrocarbons remains hypothetical.
3.15 Upper Magdalena Valley Valley Basin type
Poly-historic, rift shoulder to broken foreland
Area
26,200 km2 / 6,474,000 acres
Discovered oil reserves
631 MBO
Discovered gas reserves
123 GCF
Wildcat wells
210
Discovered elds
36
Overview
The Upper Magdalena Valley Basin of Colombia is a Neogene Broken Foreland Basin that evolved from a larger collision-related Paleogene foreland basin which extends to the east as far as the Guyana Shield. The basin has an area extend of about 26,200 km2. It is bounded on both sides by Precambrian to Jurassic basement uplifts that dene the anks of the Eastern and Central Cordillera.
The basin b asin conta contains ins a Cret Cretaceous aceous seque sequence nce that t hat star started ted with wi th contin c ontinental ental deposits followed by a transgressive sequence composed of shales and limestones, overlaid by the Caballos sandstone unit, which is one of the main reservoirs in the basin. These units are followe followed d by a seque sequence nce of limes limestones, tones, shale shales, s, and cher cherts ts of Albian to Campanian age. Two levels of organic rich source rocks of middle Albian and Turonian age provide the source of hydrocarbon for all accumulations in the basin. This sequence is overlaid by the Campanian to Maastrichtian Monserrate Formation composed mainly of sandstones. This unit is also an important hydrocarbon reservoir. The Cenozoic sequence deposited during the two collisional events that built the present day sedimentary basins in Colombia is entirely non-marine and contains Paleogene and Neogene molasses. Petroleum Geology •
Hydrocarbon Evidence
Currently, the Upper Magdalena Basin is producing 18 million barrels of oil per year from 28 elds. Numerous oil seeps abound in the basin. •
Source
Two worldwide anoxic events events of Middle Albian and Turo Turonian nian age are responsible responsible for the deposition of shales and limestones with high organic content in the Tetúan, Tetú an, Bambucá and La Luna formations. The predominant kerogen is type II. They contain on average 1%-4% of T.O.C. and Hydrogen H ydrogen index varies between 100-650 mgHc/gc. •
Migration
Migration starts soon after the rst contractional event of Late Cretaceous age and continues through today. Remigration to present day traps start during Miocene, after deposition of thick molassic deposits. •
Reservoir
Three main reservoirs are distributed distri buted in the basin. The Cretaceous Caballos and Monserrate formations and the Miocene Honda Formation, all produce from sandstone reservoirs. High reservoir potential exists in fractured carbonates. A sandy facies in the Tetúan Tetúan Fm. is a new objective for exploration; which nowadays produces in one oil led. •
Seal
Top To p and lateral seals are are provided by a very thick sequence sequence of plastic claystone of the Bambuca, Guaduala and Honda formations of Cretaceous to Neogene age. Preservation is good for the Caballos sandstone, but fair to poor for Monserrate reservoir.
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Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal
•
Trap
Structures like fault-bend fold anticlines, sub-thrust and sub-basement closures, imbricate fans, back-thrust and wrench related anticlines in both sides of the basin are all prospective. Exploration potential also exists in several types of stratigraphic traps. Trap formation began in late Cretaceous and ended by late Neogene. Time Time of initial trap formation is documented by the presence of growth strata of Maastrichtian age. •
Prospectivity
During the last two decades the basin has been actively explored for hydrocarbon. However, However, it is believed that important impor tant oil reserves remain trapped in stratigraphic and sub-thrust plays. The addition of new reserves will be linked to the development of new and maybe unconventional play concepts. More than 546 MMBO reserves have been found to date in 28 oil elds.
86
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