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首页> 外文期刊>Marine and Petroleum Geology >Petroleum generation and migration in the putumayo basin, Colombia: insights from an organic geochemistry and basin modeling study in the foothills
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Petroleum generation and migration in the putumayo basin, Colombia: insights from an organic geochemistry and basin modeling study in the foothills

机译:哥伦比亚普图马约盆地的石油产生和运移:山麓地区有机地球化学和盆地模拟研究的见解

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This paper discusses the results of 1D modeling and geochemical analyses of rock, oil and gas samples performed in the foothills of the Putumayo Basin, Colombia. A multivariate statistical assessment of biomarker data points to the existence of three oil groups, two of the them similar to oil families reported in previous studies and related to the Villeta Formation source rocks, and a novel one tentatively associated with the Caballos Formation source rocks. Geochemical data of oil and gas samples points to a complex reservoir filling history in the foothills, with at least two migration pulses with distinct maturity levels. Vitrinite reflectance data together with modeling results shows that the source rock is practically immature in the Putumayo foothills, even in the footwall of large thrust faults. The thermal and burial reconstruction of a pseudo well located in the present cordillera area suggests that the source rocks have started petroleum generation and expulsion during the Late Oligocene/Miocene. The oil and gas expelled during such a period have migrated over 80 km, reaching the present foreland area. Subsequent tectonic burial and/or higher heat flows related to the Late Miocene/Pliocene Andean Paroxysm is thought to account for a second pulse of migration of thermally evolved hydrocarbons limited to the foothills area.
机译:本文讨论了在哥伦比亚普图马约盆地山麓进行的岩石,油气样品的一维建模和地球化学分析的结果。对生物标志物数据的多变量统计评估指出,存在三个油类,其中两个与先前研究中报道的油类相似,并且与维耶塔组烃源岩有关,还有一个与卡巴洛斯组烃源岩初步相关的新型油类。石油和天然气样品的地球化学数据指出了山麓地区复杂的油藏充注历史,至少有两个具有不同成熟度水平的运移脉冲。玻璃铁矿的反射率数据和建模结果表明,即使在大冲断层的下盘下,普图马约山麓的烃源岩实际上还是不成熟的。位于当前山脉区域的一口伪井的热和埋藏重建表明,在渐新世/中新世晚期,烃源岩已经开始生出石油并驱出。在此期间驱出的石油和天然气已经迁移了80多公里,到达了目前的前陆地区。与中新世晚期/上新世安第斯阵地有关的随后的构造埋葬和/或较高的热流被认为是热生成烃运移的第二个脉动,其仅限于山麓地区。

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