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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Geochemistry and depositional environment of fresh lacustrine source rock: A case study from the Triassic Baijiantan Formation shales in Junggar Basin, northwest China
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Geochemistry and depositional environment of fresh lacustrine source rock: A case study from the Triassic Baijiantan Formation shales in Junggar Basin, northwest China

机译:新鲜湖泊源岩地球化学与沉积环境 - 以西北三角班朱根盆地三叠纪白党地层仓库案例研究

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Highlights?Sedimentary environments are low salinity to freshwater lacustrine.?Good source rocks are both Type II and Type III and mainly generate oil.?Organic matter input is derived from plankton, algae and terrestrial organisms.?Biomarkers are related to organic matter source, salinity, redox and maturation.AbstractThe shales in the Baijiantan Formation are considered to be an important potential source rock in the Junggar Basin. To evaluate this basin’s source-rock characteristics, 61 core samples from 14 boreholes were analyzed using total organic carbon and total sulfur analyses and Rock-Eval pyrolysis. Thirty-two core samples were analyzed using solvent extraction, column fractionation, biomarker analysis and the organic petrology of kerogen. The results suggest that the shales in the Baijiantan Formation have fair to excellent hydrocarbon generation potential, and the organic matter types include both Typ
机译:<![cdata [ 亮点 沉积环境对淡水湖泊盐度低盐度。 良好的源岩都是II型和类型III主要产生油。 有机质输入来自浮游生物,藻类和陆生物。 生物标志物与有机物源,盐度,红色有关牛和成熟。 抽象 Baijiantan形成中的Shales被认为是Junggar流域的重要潜在源岩。为了评估该盆地的源岩特性,使用总有机碳和总硫分析和岩析热解,分析来自14个钻孔的61个核心样品。使用溶剂萃取,柱分馏,生物标志物分析和Kerogen的有机探测器分析了三十二个核心样品。结果表明,白利坦组中的Shales具有优异的碳氢化合物产生潜力,有机物质类型包括典型

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