Petroleum system modeling in the Eastern Cordillera of Colombia using geochemistry and timing of thrusting and deformation (Record no. 191356)

MARC details
000 -LEADER
fixed length control field 03345nab a2200289 4500
008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL
Campo de control de longitud fija 260224s2015 xxu ing
041 ## - IDIOMA
Idioma Inglés
245 00 - TITULO
Título Petroleum system modeling in the Eastern Cordillera of Colombia using geochemistry and timing of thrusting and deformation
260 ## - PUBLICACION, DISTRIBUCION, ETC
Lugar de publicación, distribución, etc.
Nombre de publicador, distribuidor, etc.
Fecha de publicación, distribución, etc. ago. 2015
270 ## - FECHA DE CARGA
Fecha de carga 17/10/2017 ; 17/10/2017
300 ## - DESCRIPCION FISICA
Otra extensión 19 p. ; 1537-1556
520 ## - RESUMEN, ETC
Resumen Transcripción del resumen del autor: In the present study, stratigraphic data from cores and outcrop sections are integrated with data on thermal maturity, organic facies, and thermochronometric information to reconstruct the tectonic and associated Previous HitpetroleumNext Hit Previous HitsystemNext Hit evolution of the Previous HiteasternNext Hit foothills thrust belt along the Colombian Previous HitEasternNext Hit Previous HitCordilleraNext Hit, one of the most prolific hydrocarbon provinces in northern South America. Sedimentary and tectonic burial of the foreland autochthon caused maturation of the Coniacian to Santonian shallow marine Chipaque Formation, resulting in successive and diachronous episodes of hydrocarbon migration and trapping. One-dimensional and two-dimensional maturation Previous HitmodelingNext Hit indicates that oil generation from the Chipaque Formation began at the Paleocene-Eocene boundary (55 Ma) in the southern parts of what is now the Previous HitEasternNext Hit Previous HitCordilleraNext Hit and progressed to the north. By the late Oligocene, tectonic inversion of the Previous HitEasternNext Hit Previous HitCordilleraNext Hit exhumed most of these kitchens, terminating the oil generation from the Chipaque Formation. Kitchens migrated northward and eastward during the Oligocene and early Miocene. Because of the absence or subsequent erosion of traps, it is likely that the southernmost source rocks expelled most of their oil without any appreciable accumulation. Our Previous HitmodelingNext Hit indicates that there were two important kitchens during the Cenozoic. The larger of the two was located in the present-day Previous HitEasternNext Hit Previous HitCordilleraNext Hit, and it was most productive in the late Eocene–early Oligocene. The second kitchen, which generated oil throughout the Neogene, was located in the foredeep of the Llanos basin, adjacent to the mountain front. Considerable amounts of oil from this recent pulse have accumulated in both deep and shallow reservoirs along the Previous HiteasternTop foothills. The modeled reservoir charge history also explains the substantial biodegradation of oils in reservoirs that are today much too deep to support the process. Biodegradation must have occurred when the reservoirs were shallower and at cooler temperatures, and they remained active until the reservoirs were buried to depths where temperatures were high enough to prevent further bacterial activity.
581 ## - ESTADO DE COLECCIÓN
Estado de colección 8
773 0# - CORRECCIÓN
Título AAPG Bulletin
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942 ## - DESC. DE MATERIAL
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Holdings
Biblioteca propietaria Biblioteca actual Fecha de adquisición Inventario Total de préstamos Inventario Fecha de carga Tipo de item KOHA
Biblioteca Alejandro Angel Bulgheroni Biblioteca Alejandro Angel Bulgheroni 06/03/2026 200063631   200063631 06/03/2026 Artículo de Revista


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