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Jurassic paleogeography of the West Siberian sedimentary basin

机译:西西伯利亚沉积盆地的侏罗纪古地理

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摘要

Paleogeographic reconstruction of the West Siberian basin during the Jurassic is based on a variety of criteria used to evaluate the depositional environments (paleontological, sedimentological, geochemical, etc.). Extensive geochemical data on the hydrocarbon biomarkers in bitumen from organic matter are first used to constrain the depositional setting of this large region over a span of about 45 Myr. The study provides a detailed description of paleogeographic maps compiled for the main epochs of the Jurassic period with the reconstruction of paleorelief and differentiation of potential external and internal sources of terrigenous material. The paleogeographic reconstructions of the basin are considered with implications for the formation of regional seals and reservoir units. A special emphasis is given to interpretation of organic matter type and depositional setting of the major oil and gas source rocks. The study infers a paleogeographic control on the stratigraphic and areal distribution of hydrocarbon accumulations in the basin.
机译:侏罗纪时期西西伯利亚盆地的古地理重建基于各种用于评估沉积环境(古生物学,沉积学,地球化学等)的标准。首先使用有关有机物质中沥青中碳氢化合物生物标志物的广泛地球化学数据来约束这个大区域在约45 Myr跨度上的沉积环境。这项研究详细描述了为侏罗纪主要时期编制的古地理图,其中包括重建古地理和区分陆源物质的潜在外部和内部来源。考虑到该盆地的古地理重建对区域封存和储层单元的形成具有重要意义。特别强调解释主要油气源岩的有机质类型和沉积环境。该研究推论了该盆地油气成藏的地层和面积分布的古地理控制。

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