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Geochemical evaluation of southern Tampico-Misantla Basin, Mexico: Oil-oil and oil source rock correlations.

机译:墨西哥南部坦皮科-米桑特拉盆地的地球化学评价:石油与石油和岩石的相关性。

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摘要

The bulk of the oil in the southern Tampico-Misantla Basin is in Upper Cretaceous reservoirs of the Golden Lane and Poza Rica Trend, with additional production from Upper Jurassic and Eocene reservoirs. The nature of the source rocks that gave rise to these oils is not known. This study presents results of geochemical characterization of oils and possible source rocks from the Tertiary, Cretaceous, and Upper Jurassic formations of the study area. Oil-oil and oil-source rock correlations are based on analyses of n-alkanes, isoprenoids, stable carbon isotopes, and biomarkers in oils and rock extracts.;The data indicate that the Tertiary formations are thermally immature and poor source rocks. Cretaceous formations have entered the oil window and are fair source rocks, whereas Upper Jurassic formations, namely, the Santiago, Taman, and Pimienta Formations, are good source rocks in the early stage of oil generation. Upper Jurassic Formations in the study area consist of shales and carbonates, and were deposited in environments from suboxic to anoxic.;Analyses of the oils suggest that they have a common origin and that they were generated from an organic carbon-rich carbonate source rock containing algal and bacterial organic matter deposited in an anoxic environment. The physical and chemical differences among oils are explained by migration effects, thermal maturation differences, changes of organic facies of the source rock, and contamination during migration through younger rocks. Oils display geochemical similarities to Upper Jurassic carbonate source rocks. However, it is difficult to correlate oils and rocks in the study area. Therefore, it is possible that the studied Upper Jurassic-Cretaceous section has not contributed significantly to the oils entrapped locally. These data and geological considerations imply that oils have migrated from deeper facies downdip of the study area, most likely from offshore Gulf of Mexico.
机译:Tampico-Misantla盆地南部的大部分石油位于Golden Lane和Poza Rica Trend的上白垩统储层,而上侏罗纪和始新世储层还有额外的产量。产生这些油的烃源岩的性质未知。这项研究提出了研究区域第三纪,白垩纪和上侏罗统地层的石油和可能的烃源岩的地球化学特征。石油与油源岩的相关性是基于对油和岩石提取物中正构烷烃,类异戊二烯,稳定的碳同位素以及生物标志物的分析得出的。数据表明,第三系地层是热不成熟的烃源岩。白垩纪地层已进入油窗,是公平的烃源岩,而上侏罗统地层,即圣地亚哥,塔曼和Pimienta地层,是早期生油的良好烃源岩。研究区的上侏罗统地层由页岩和碳酸盐组成,沉积在从低氧到缺氧的环境中;对这些油的分析表明它们具有共同的起源,并来自于富含碳的有机碳酸盐岩。在缺氧环境中沉积的藻类和细菌有机物。油之间的物理和化学差异可以通过运移效应,热成熟差异,烃源岩有机相的变化以及在通过年轻岩石的运移过程中的污染来解释。石油显示出与上侏罗统碳酸盐岩的地球化学相似性。但是,很难将研究区域中的石油和岩石关联起来。因此,研究的上侏罗统-白垩纪剖面可能对当地滞留的油没有显着贡献。这些数据和地质考虑因素表明,石油是从研究区较深的下倾角迁移的,最有可能是从墨西哥湾的近海迁移的。

著录项

  • 作者单位

    The University of Texas at Dallas.;

  • 授予单位 The University of Texas at Dallas.;
  • 学科 Engineering Petroleum.;Geochemistry.
  • 学位 Ph.D.
  • 年度 1996
  • 页码 632 p.
  • 总页数 632
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 康复医学;
  • 关键词

  • 入库时间 2022-08-17 11:49:20

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