Llanos Basin
| Llanos Basin | |
|---|---|
| Cuenca Llanos | |
 The Llanos Basin in Puerto López, Meta | |
| Coordinates | 05°24′00″N 71°40′00″W / 5.40000°N 71.66667°W |
| Etymology | Llanos Orientales Spanish: "eastern plains" |
| Region | Orinoquía |
| Country |  Colombia |
| State(s) | Arauca, Boyacá, Casanare, Cundinamarca, Guainía, Guaviare, Meta, Norte de Santander |
| Cities | Villavicencio, Yopal |
| Characteristics | |
| On/Offshore | Onshore |
| Boundaries | Colombia-Venezuela border (N), Guiana Shield (E), Vaupés Arch (S), Serranía de la Macarena (SW), Eastern Ranges (W) |
| Part of | Andean foreland basins |
| Area | 96,000 km2 (37,000 sq mi) |
| Hydrology | |
| River(s) | Orinoco watershed Main rivers: Arauca, Meta, Guaviare, Vichada |
| Geology | |
| Basin type | Foreland on rift basin[note 1] |
| Plate | South American[note 3] |
| Orogeny | Break-up of Pangea (Mesozoic) Andean (Cenozoic) |
| Age | Paleozoic or Jurassic[note 2] to Holocene |
| Stratigraphy | Stratigraphy |
| Faults | Eastern (W, bounding), Chichimene & Meta |
| Field(s) | Rubiales, Caño Limón, many more |
The Llanos Basin (Spanish: Cuenca Llanos) or Eastern Llanos Basin (Spanish: Cuenca de los Llanos Orientales) is a major sedimentary basin of 96,000 square kilometres (37,000 sq mi) in northeastern Colombia. The onshore foreland on Mesozoic rift basin covers the departments of Arauca, Casanare and Meta and parts of eastern Boyacá and Cundinamarca, western Guainía, northern Guaviare and southeasternmost Norte de Santander. The northern boundary is formed by the border with Venezuela, where the basin grades into the Barinas-Apure Basin.
Description
[edit]The northeastern part of Colombia is characterized by its wavy plains, called Llanos Orientales, as part of the bigger Llanos that extend into Venezuela. The landscape is similar to a savanna and is poor in trees. It is located between the Eastern Ranges of the Colombian Andes in the west, the Vaupés Arch in the south and the Guiana Shield in the east.[1]
Geologically, the Llanos Basin underlies this typical landscape of the Llanos. An area where transport occurs mostly by small boats along the many rivers and the "buses of the Llanos", the Douglas DC-3 planes. The basin covers an area of 96,000 square kilometres (37,000 sq mi) and contains a stratigraphic column from the Paleozoic to recent.[2] Several of the formations in the basins are source rocks (Gachetá, Los Cuervos, Carbonera C8), reservoir rocks (Mirador, Barco, Guadalupe and the uneven numbered members of Carbonera). Seals are formed by the shaly intervals (even numbered) of the Carbonera Formation, Los Cuervos, and León.[3]
The basin is the main petroleum producing basin of Colombia, with four of the nations biggest oil fields located in the Llanos Basin. Major fields are Rubiales, Colombia's biggest and most recent giant discovery sealed by a complex of hydrodynamic processes, and Caño Limón, at the border with Venezuela.
Major concerns in the basin for the production of petroleum are biodegradation, hydrocarbon migration, fault seal capacity and water flow.
Hydrography
[edit]
The Llanos Basin is crossed by numerous rivers, all belonging to the Orinoco watershed. From north to south:
Flora and fauna
[edit]Fauna
[edit]
Among other species, Lynch's swamp frog (Pseudopaludicola llanera) is endemic to the Llanos, with the species epithet referring to the plains.[4] Also the whip scorpion Mastigoproctus colombianus is reported from the Llanos Basin.[5]
Geodynamic situation
[edit]
Nazca Plate has been subdivided into Coiba and Malpelo Plates
The country of Colombia spreads out over six tectonic plates, clockwise from north:
The Llanos Basin is situated entirely on the South American Plate, bordering the North Andean Block or North Andean microplate in the west. The basin is one of three Colombian basins on the South American Plate, to the south the Caguán-Putumayo Basin and to the southeast the Vaupés-Amazonas Basin. The northern boundary of the Llanos Basin is formed by the Colombia-Venezuela border where the basin grades into the Barinas-Apure Basin on the Venezuelan side. The Catatumbo Basin, representing the Colombian portion of the larger Maracaibo Basin borders the Llanos Basin in the northwest and the western boundary is formed by the foothills (Piedemonte) of the Eastern Cordillera Basin, the sedimentary basin covering the Eastern Ranges of the Colombian Andes.
Tectonics
[edit]The basin is bound to the west by the Eastern Frontal Fault System, a 921.4 kilometres (572.5 mi) long fault system connecting the North Andes and South American Plates and thus the Eastern Cordillera Basin and the Llanos Basin. The fault system has an average strike of 042.1±19, but this orientation varies greatly along its course. The 1827, 1834, 1917, 1967, 1995, and 2008 earthquakes were all caused by fault movement as part of the system.[6]
Basin history
[edit]The tectonic history of the Llanos Basin, a foreland basin formed on top of Mesozoic rift basins, Paleozoic metasediments and Precambrian basement underlain by continental crust, goes back to the Early Jurassic.
The Andean orogeny, represented by the tectonic uplift of the Colombian Eastern Ranges and its northern extension, the Serranía del Perijá, caused tilting and uplift in the Llanos Basin. During the Andean orogenic phase, the paleotemperatures in the basin dropped considerably; in the Baja Guajira area from 115 °C (239 °F) in the Early Miocene to 70 °C (158 °F) in the Late Miocene.[7] In the Late Miocene to Pliocene, the major faults to the southwest of the Cocinetas Basin, the Oca and Bucaramanga-Santa Marta Faults were tectonically active.[8]
Basement
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The stratigraphy of the Llanos Basin ranges, depending on the definition from either Jurassic or Paleozoic to recent. The basement is formed by the westernmost extensions of the Guiana Shield. Remnants of these Precambrian formations are found as inselbergs in the far east of Colombia (Cerros de Mavecure), in the Serranía de la Macarena to the southwest of the basin and in the tepuis of the Serranía de Chiribiquete to the southeast.
The Proterozoic crystalline rocks are overlain by metamorphosed sedimentary and igneous rocks ranging in age from Cambrian to Devonian. Younger and contemporaneous Paleozoic deposits are only found in the subsurface and in regional correlative units as the Floresta and Cuche Formations of the Altiplano Cundiboyacense to the direct northwest and the Río Cachirí Group of the Cesar-Ranchería Basin farther northwest of the Llanos Basin.
The units found in the Llanos Basin pertain to the Farallones Group and comprise the Valle del Guatiquía Red Beds, Pipiral Shale and the Gutiérrez Sandstone.[9]
Stratigraphy
[edit]
- Legend
- group
- important formation
- fossiliferous formation
- minor formation
- (age in Ma)
- proximal Llanos (Medina)[note 4]
- distal Llanos (Saltarin 1A well)[note 5]
Paleozoic
[edit]- Cambro-Ordovician
- Pre-Devonian
- Devonian
Jurassic
[edit]Petroleum geology
[edit]The Llanos Basin is the most prolific hydrocarbon basin of Colombia, hosting well-known petroleum deposits as Caño Limón, Rubiales and other fields. Nine of the twenty most producing oil fields of Colombia are situated in the Llanos Basin.
Fields
[edit]Based on data released in March 2018, Colombia is the 21st oil producer in the world. Daily production dropped in 2017 to 854.121 thousand barrels per day (135.7944×103 m3/d).[50] In 2016, twenty oilfields produced 66% of all oil of Colombia, listed below in bold.[51] The total proven reserves of Colombia were 1,665.489 million barrels (264.7916×106 m3) in 2016.[52]
Major oil fields in the Llanos Basin are:[53]
| Name | Map | Location | Operator | Reservoirs | Reserves Production (2016) | Notes |
|---|---|---|---|---|---|---|
| Rubiales |  | Puerto Gaitán Meta | Ecopetrol | Carbonera 7 | 4,380 million bbl (696 million m3) 132.000 kbbl/d (20.9863×103 m3/d) | |
| Castilla |  | Castilla la Nueva Meta | Ecopetrol | Mirador Gachetá Une | 452 million bbl (71.9 million m3) 121.363 kbbl/d (19.2952×103 m3/d) | [54][55] |
| Chichimene |  | Acacias Meta | Ecopetrol | Mirador Guadalupe Gachetá Une | 74.052 kbbl/d (11.7733×103 m3/d) | [56][57] |
| Quifa | | Puerto Gaitán Meta | Meta Petroleum | Carbonera | 613 million bbl (97.5 million m3) 46.557 kbbl/d (7.4020×103 m3/d) | [58][59] |
| Caño Limón |  | Puerto Rondón Arauca | Ecopetrol | 20.930 kbbl/d (3.3276×103 m3/d) | [60] | |
| Avispa |  | Cabuyaro Meta | Pacific Rubiales | 11.625 kbbl/d (1.8482×103 m3/d) | ||
| Ocelote | | Puerto Gaitán Meta | Hocol | 11.228 kbbl/d (1.7851×103 m3/d) | ||
| Chipirón | | Puerto Rondón Arauca | OXY | 10.459 kbbl/d (1.6628×103 m3/d) | [59] | |
| Jacana |  | Villanueva Casanare | Geopark | 7.477 kbbl/d (1.1887×103 m3/d) | ||
| Cupiagua |  | Aguazul Casanare | Ecopetrol | 5.358 kbbl/d (851.9 m3/d) | ||
| Apiay |  | Villavicencio Meta | Ecopetrol | Gachetá Une | ||
| Arauca |  | Arauca Arauca | Ecopetrol | |||
| Cusiana |  | Tauramena Casanare | Ecopetrol | Mirador Barco Guadalupe |
- Other fields[53]
- Caño Verde
- Chaparrito
- Concesión
- Corcel
- Cravo Sur
- La Gloria
- Santiago
- Trinidad
- Valdivia
Mining
[edit]Mining activities in the Llanos Basin are restricted to certain areas, resulting in less conflicts, more common with indigenous peoples in the Amazonian part of Colombia.[61]
In San José del Guaviare platinum is mined.[65]
| Resources | Map | Department | Municipality | Mine | Notes |
|---|---|---|---|---|---|
| halite |  | Meta | Restrepo | Upín | [63][66] |
| gold |  | Puerto Rico | [62] | ||
| Arauca | Arauca | |||
| gold |  | Guaviare | San José del Guaviare | ||
| platinum, iron, albite, andradite (var: melanite), 'apatite', arfvedsonite, 'biotite', calcite, cancrinite, epidote, fluorite, 'garnet', microcline, 'monazite', nepheline, siderite, titanite, zircon | [65][67] | ||||
| coal |  | Casanare | Recetor | [64] |
Paleontology
[edit]
NeogeneH = Honda Group
Co = Cocinetas Basin
PaleogeneB = Bogotá
C = Cerrejón
CretaceousL = La Frontera
P = Paja
JurassicJ = Valle Alto
DevonianF = Cuche and Floresta
Cambro-OrdovicianM = Duda, La Macarena
Compared to many fossiliferous formations in Colombia, the Llanos Basin has been lean in fossil content. Most of the basin stratigraphy is only known from wells.
Paleozoic outcrops surrounding and perforating the planar geography have provided fossils dating back to the Cambrian; the Duda and Ariarí Formations.
Several fossiliferous formations of contemporaneous depositional environments have provided many unique fossils indicative of paleoclimatic conditions; turtle fossils were described from Los Cuervos in the Cesar-Ranchería Basin, and the Mirador Formation in the Catatumbo Basin direct northwest of the Llanos Basin has provided many fossil flora.[68]
- Other correlative units with surrounding basins
- Guayabo - Sabana and Soatá, Ware, Honda
- León - Honda
- Carbonera - Barzalosa, Castilletes, Jimol
- Mirador - Bogotá - Etayoa
- Los Cuervos - Cerrejón - Titanoboa, crocodylians, turtles, flora
- Los Cuervos - Guaduas - fossil flora
- Gachetá - Chipaque - oysters
- Gachetá - La Luna - many
- Une - Hiló - ammonites
- Farallones Group - Floresta and Cuche
See also
[edit]- Sedimentary basins of Colombia
- Neuquén Basin, major petroleum producing basin of Argentina
- Santos Basin, major petroleum producing basin of Brazil
- Eastern Venezuela Basin, primary petroleum producing basin of Venezuela
Sources
[edit]Notes
[edit]- ^ More detailed: continental margin (Protero- and Paleozoic), rift basin (Mesozoic), foredeep (Paleogene and early Neogene), foreland (late Neogene to recent)
- ^ Depending on the definition of basement, the stratigraphic succession starts either in the Paleozoic on Proterozoic crystalline basement or Jurassic on top of both
- ^ The northernmost of three Colombian basins on this plate, to the south the Caguán-Putumayo and Vaupés-Amazonas Basins
- ^ based on Duarte et al. (2019)[46], García González et al. (2009),[47] and geological report of Villavicencio[48]
- ^ based on Duarte et al. (2019)[46] and the hydrocarbon potential evaluation performed by the UIS and ANH in 2009[49]
References
[edit]- ^ Barrero et al., 2007, p.69
- ^ ANH, 2010
- ^ García González et al., 2009, p.58
- ^ Pseudopaludicola llanera at IUCN.org
- ^ Mastigoproctus colombianus at GBIF.org
- ^ Paris et al., 2000a, p.36
- ^ Hernández Pardo et al., 2009, p.122
- ^ Hernández Pardo et al., 2009, p.28
- ^ Plancha 266, 1998
- ^ a b c d e f García González et al., 2009, p.27
- ^ a b c d e f García González et al., 2009, p.50
- ^ a b García González et al., 2009, p.85
- ^ a b c d e f g h i j Barrero et al., 2007, p.60
- ^ a b c d e f g h Barrero et al., 2007, p.58
- ^ Plancha 111, 2001, p.29
- ^ a b Plancha 177, 2015, p.39
- ^ a b Plancha 111, 2001, p.26
- ^ Plancha 111, 2001, p.24
- ^ Plancha 111, 2001, p.23
- ^ a b Pulido & Gómez, 2001, p.32
- ^ Pulido & Gómez, 2001, p.30
- ^ a b Pulido & Gómez, 2001, pp.21-26
- ^ Pulido & Gómez, 2001, p.28
- ^ Correa Martínez et al., 2019, p.49
- ^ Plancha 303, 2002, p.27
- ^ Terraza et al., 2008, p.22
- ^ Plancha 229, 2015, pp.46-55
- ^ Plancha 303, 2002, p.26
- ^ Moreno Sánchez et al., 2009, p.53
- ^ Mantilla Figueroa et al., 2015, p.43
- ^ Manosalva Sánchez et al., 2017, p.84
- ^ a b Plancha 303, 2002, p.24
- ^ a b Mantilla Figueroa et al., 2015, p.42
- ^ Arango Mejía et al., 2012, p.25
- ^ Plancha 350, 2011, p.49
- ^ Pulido & Gómez, 2001, pp.17-21
- ^ Plancha 111, 2001, p.13
- ^ Plancha 303, 2002, p.23
- ^ Plancha 348, 2015, p.38
- ^ Planchas 367-414, 2003, p.35
- ^ Toro Toro et al., 2014, p.22
- ^ Plancha 303, 2002, p.21
- ^ a b c d Bonilla et al., 2016, p.19
- ^ Gómez Tapias et al., 2015, p.209
- ^ a b Bonilla et al., 2016, p.22
- ^ a b Duarte et al., 2019
- ^ García González et al., 2009
- ^ Pulido & Gómez, 2001
- ^ García González et al., 2009, p.60
- ^ Producción de crudo bajó en 30.879 barriles por día en 2017 - El Tiempo
- ^ En 20 campos se produce el 66 % del petróleo del país - El Tiempo
- ^ Oil reserves per department - 2016 - ANH
- ^ a b Mojica et al., 2009, p.30
- ^ ANH & Halliburton, s.a., p.2
- ^ Castilla, área petrolera especial - El Tiempo
- ^ ANH & Halliburton, s.a., p.3
- ^ Chichimene
- ^ Las reservas de campo Quifa se reducen en 5,9 millones de barriles
- ^ a b Mapa de Tierras, ANH, 2017
- ^ Caño Limón
- ^ (in Spanish) Mapa de Territorios Indígenas y Minerales Preciosos
- ^ a b (in Spanish) Producción de oro – UPME
- ^ a b (in Spanish) Producción de sal – UPME
- ^ a b (in Spanish) Producción de carbón – UPME
- ^ a b (in Spanish) Producción de platino – UPME
- ^ Upin at Mindat.org
- ^ San José del Guaviare at Mindat.org
- ^ Jaramillo & Dilcher, 2001
Bibliography
[edit]General
[edit]- Barrero, Dario; Pardo, Andrés; Vargas, Carlos A.; Martínez, Juan F. (2007), Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal, ANH, pp. 1–92
- García González, Mario; Mier Umaña, Ricardo; Cruz Guevara, Luis Enrique; Vásquez, Mauricio (2009), Informe Ejecutivo - evaluación del potencial hidrocarburífero de las cuencas colombianas, Universidad Industrial de Santander, pp. 1–219
Hydrodynamics
[edit]- Mora, Andrés; Gómez, Ricardo Andrés; Díaz, Camilo; Caballero, Victor; Parra, Mauricio; Villamizar, Carlos; Lasso, Álvaro; Ketcham, Richard A.; González Penagos, John Rico and Juan Pablo Arias Martínez, Felipe (2019), "Water flow, oil biodegradation, and hydrodynamic traps in the Llanos Basin, Colombia", AAPG Bulletin, 103 (5): 1225–1264, Bibcode:2019BAAPG.103.1225M, doi:10.1306/1003181611317237, retrieved 2019-10-26
- Duarte, Edward; Bayona, German; Jaramillo, Carlos; Parra, Mauricio; Romero, Ingrid; Mora, Josué Alejandro (2017), "Identificación de los máximos eventos de inundación marina Miocenos y su uso en la correlación y análisis de la cuenca de antepaís de los Llanos Orientales, Colombia", Boletín de Geología, 39: 19–40, doi:10.18273/revbol.v39n1-2017001, retrieved 2019-10-26
- Bartha, Attila; De Nicolais, Nelly; Sharma, Vinod; Roy, S.K.; Srivastava, Rajiv; Pomerantz, Andrew E.; Sanclemente, Milton; Pérez, Wilmar; Nelson, Christopher M. Reddy, Jonas Gros, J. Samuel Arey, Jaron Lelijveld, Sharad Dubey, Diego Tortella, Thomas Hantschel, Kenneth E. Peters and Oliver C. Mullins, Robert K. (2015), "Combined Petroleum System Modeling and Comprehensive Two-Dimensional Gas Chromatography To Improve Understanding of the Crude Oil Chemistry in the Llanos Basin, Colombia", Energy & Fuels, American Chemical Society, 29 (8): 4755–4767, doi:10.1021/acs.energyfuels.5b00529, retrieved 2019-10-26
{{citation}}: CS1 maint: multiple names: authors list (link) - Gómez Galarza, Yohaney; Yoris, Franklin; Rodríguez, Javier; Portillo, Fredy; Araujo, Ysidro (2010), "Aspectos hidrodinámicos, estructurales y estratigráficos del Campo Rubiales" (PDF), Geo Petróleo, 9: 1–28, retrieved 2017-06-07
- Gómez, A.; Jaramillo, C.; Parra, M.; Mora, A. (2009), "Huesser Horizon: A lake and marine incursion in Northwestern South America during the Early Miocene", PALAIOS, 24 (4): 199–210, Bibcode:2009Palai..24..199G, doi:10.2110/palo.2007.p07-074r, retrieved 2019-10-26
Tectonics
[edit]- Paris, Gabriel; Machette, Michael N.; Dart, Richard L.; Haller, Kathleen M. (2000a), Map and Database of Quaternary Faults and Folds in Colombia and its Offshore Regions (PDF), USGS, pp. 1–66, retrieved 2017-09-18
- Paris, Gabriel; Machette, Michael N.; Dart, Richard L.; Haller, Kathleen M. (2000b), Map of Quaternary Faults and Folds of Colombia and Its Offshore Regions (PDF), USGS, p. 1, retrieved 2017-09-18
Petroleum
[edit]- Martínez Sánchez, Dilan; Jiménez, Giovanny (2019), "Hydraulic fracturing considerations: Insights from analogue models, and its viability in Colombia", Earth Sciences Research Journal, 23: 5–15, doi:10.15446/esrj.v23n1.69760, retrieved 2019-10-26 ISSN 1794-6190
- Vargas Jiménez, Carlos A (2012), "Evaluating total Yet-to-Find hydrocarbon volume in Colombia", Earth Sciences Research Journal, 16: 1–290
- Mojica, Jairo; Arévalo, Oscar J.; Castillo, Hardany (2009), Cuencas Catatumbo, Cesar – Ranchería, Cordillera Oriental, Llanos Orientales, Valle Medio y Superior del Magdalena (PDF), ANH, pp. 1–65, retrieved 2017-06-14
- Piedrahita, Carlos; Montaña, Clara L. (2007), "Methodology implemented for the 3D-Seismic modelling using GoCad and NORSAR 3D Software applied to complex areas in the Llanos foothills", Earth Sciences Research Journal, 11: 35–43, retrieved 2019-10-26
- Hernández Pardo, Orlando; von Frese, Ralph R.B.; Woo Kim, Jeong (2007), "Crustal thickness variations and seismicity of northwestern South America", Earth Sciences Research Journal, 11: 81–94, retrieved 2019-10-26
- N., N (2006), Cuenca Llanos Orientales - Estudio Integrado - Crudos Pesados (PDF), ANH, pp. 1–10, retrieved 2017-06-07
Paleontology
[edit]- Jaramillo, Carlos A.; Dilcher, D.L. (2001), "Middle Paleogene palynology of Central Colombia, South America: A study of pollen and spores from tropical latitudes", Palaeontographica Abteilung B, 258 (4–6): 87–213, Bibcode:2001PalAB.258...87J, doi:10.1127/palb/258/2001/87, retrieved 2019-10-26
Reports
[edit]- Pinto Valderrama, Jorge Eduardo; Mora Ortiz, José Pedro; Reátiga Tarazona, Gloria; Rey Pilonieta, Jorge Alberto; Toloza Hormiga, Silvia Johana; Torres Coronado, Diego Andrés; Vargas Mojica, David Ricardo; Zafra Manrique, Cristian Julián (2010), Geología del Piedemonte Llanero en la Cordillera Oriental, departamentos de Arauca y Casanare (PDF), INGEOMINAS & Universidad Industrial de Santander, pp. 1–64, retrieved 2017-08-04
- Terraza, Roberto; Montoya, Diana; Reyes, Germán; Moreno, Giovanni; Fúquen, Jaime; Torres Jaimes, Eliana; López Cardona, Myriam; Nivia Guevara, Álvaro; Etayo Serna, Fernando (2013), Geología de la Plancha 229 - Gachalá - 1:100,000 (PDF), Servicio Geológico Colombiano, pp. 1–296, retrieved 2017-08-04
- Patiño, Alejandro; Fuquen, Jaime; Ramos, Julián; Pedraza, Andrea; Ceballos, Leonardo; Pinzón, Lyda; Jerónimo, Yadira; Álvarez, Leidy; Torres, Andrea (2011), Cartografía geológica de la Plancha 247 - Cáqueza - 1:100,000 (PDF), INGEOMINAS, retrieved 2017-08-04
- Acosta, Jorge E.; Ulloa, Carlos E. (2002), Mapa geológico del Departamento de Cundinamarca 1:250,000 - Memoria Explicativa, INGEOMINAS, pp. 1–108
- Pulido, Orlando; Gómez, Luz Stella (2001), Geología de la Plancha 266 - Villavicencio - 1:100,000, INGEOMINAS, pp. 1–52
Maps
[edit]- ANH (2017), Mapa de Tierras (PDF), ANH, p. 1, retrieved 2018-06-02
- Departmental
- Reyes, Germán; Cardozo, Ana Milena (1999), Mapa Geológico de Arauca 1:250,000, INGEOMINAS, p. 1, retrieved 2017-09-21
- Acosta, Jorge; Ulloa, Carlos; García, Pilar; Solano, Orlando (1999), Mapa Geológico de Cundinamarca, INGEOMINAS, p. 1, retrieved 2017-09-21
- Rodríguez, Antonio José (2002), Mapa Geológico del Meta 1:500,000, INGEOMINAS, p. 1, retrieved 2017-09-21
- Local
- Fúquen, Jaime; Ceballos, Leonardo; Pedraza, Andrea; Marín, Edwin (2010), Plancha 99 - Villa del Rosario - 1:100,000 (PDF), INGEOMINAS, p. 1, retrieved 2018-06-01
- Royero, José María; Zambrano, J.; Daconte, Rommel; Mendoza, H.; Vargas, Rodrigo (1999), Plancha 111 - Toledo - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- Daconte B., Rommel; Salinas E, Rosalba (1982), Plancha 122 - Río Cobugón - 1:100,000 (PDF), INGEOMINAS, p. 1, retrieved 2018-06-01
- Vargas, Rodrigo; Arias, Alfonso; Jaramillo, Luis; Tellez, Noel (1984), Plancha 136 - Málaga - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- López, Carolina; Dávila, Camilo; González, Francisco; Parra, Eduardo; Chaquea, Claudia; Ojeda, Carolina; Q., Carlos; Espinel, Valentina; Lancheros, José A. (2011), Plancha 139 - Betoyes - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- López, Carolina; Dávila, Camilo; González, Francisco; Parra, Eduardo; Chaquea, Claudia; Ojeda, Carolina; Q., Carlos; Espinel, Valentina; Lancheros, José A. (2011), Plancha 155 - Puerto Rondón - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- Ulloa, Carlos E.; Rodríguez, Erasmo; Escovar, Ricardo (1998), Plancha 192 - Laguna de Tota - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- Terraza, Roberto; Moreno, Giovanni; Buitrago, José A.; Pérez, Adrián; Montoya, Diana María (2010), Plancha 210 - Guateque - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- Buitrago, José Alberto; Terraza M., Roberto; Etayo, Fernando (1998), Plancha 228 - Santafé de Bogotá Noreste - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- Ulloa, Carlos E; Escovar, Ricardo; Pacheco, Adolfo H. (2009), Plancha 230 - Monterrey - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- Acosta, Jorge; Calcedo, Juan Carlos; Ulloa, Carlos (1999), Plancha 265 - Icononzo - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- Pulido, Orlando; Gómez, Luz Stella; Marín, Pedro (1998), Plancha 266 - Villavicencio - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- Duarte, Rafael; Moreno, Mauricio; Morales, Carlos Julio; Villegas, Henry; Alvarado, Sonia; Téllez, Milena; Pacheco, Sonia; Rojas, Nadia (2010), Plancha 267 - Pachaquiaro - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- Unión Temporal, G&H (2015), Plancha 284 - Santana - 1:100,000 (PDF), Servicio Geológico Colombiano, p. 1, retrieved 2018-06-01
Further reading
[edit]- Bally, A.W.; Snelson, S. (1980), "Realms of subsidence", Canadian Society for Petroleum Geology Memoir, 6: 9–94
- Kingston, D.R.; Dishroon, C.P.; Williams, P.A. (1983), "Global Basin Classification System" (PDF), AAPG Bulletin, 67: 2175–2193, retrieved 2017-06-23
- Klemme, H.D (1980), "Petroleum Basins - Classifications and Characteristics", Journal of Petroleum Geology, 3 (2): 187–207, Bibcode:1980JPetG...3..187K, doi:10.1111/j.1747-5457.1980.tb00982.x
Sedimentary basins of Colombia | ||||||||
|---|---|---|---|---|---|---|---|---|
| Onshore |
|      | ||||||
| Offshore | ||||||||
| Source | Barrero, Dario; Pardo, Andrés; Vargas, Carlos A.; Martínez, Juan F. (2007). Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal. ANH. pp. 1–92. | |||||||
