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Geochemical characterization of source rocks and crude oils in the Upper Cretaceous Qingshankou Formation, Chang ling Sag, southern Songliao Basin

机译:松辽盆地南部长岭凹陷上白垩统青山口组烃源岩和原油的地球化学特征

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The Upper Cretaceous Qingshankou Formation is one of the main exploration target in the Changling Sag, southern Songliao Basin. However, the origin of source rock deposition and crude oils remains undiscovered. A comprehensive geochemical study, including Rock-Eval pyrolysis, gas chromatography-mass spectrometry and carbon isotope analysis on fifteen crude oils and twenty-two source rock samples from the Qingshankou Formation were performed in order to provide new insights into source organic matter, depositional environment and correlation between crude oils and source rocks.Bulk geochemical analysis on source rock samples indicates that the lower member of the Qingshankou Formation has more hydrocarbon generating potential than the middle member. These two potential source rock members were interpreted to be deposited in slightly different environments and have different sources of organic matter determined by biomarker assemblages. The lower member is organically rich (average TOC = 1.27 wt.%), oil-prone, mature and deposited under anoxic conditions with more contribution from sapropelic organic matter. The middle member is organically poor (average TOC = 0.78 wt.%), gas-prone, less mature and deposited under less anoxic conditions with more terrigenous organic matter input. Biomarker fingerprints and carbon isotope compositions suggest that all the crude oils were genetically related and could be classified into one oil family, which has significant contribution from the lower member source rocks and minor contribution from the middle member source rocks. (C) 2015 Elsevier Ltd. All rights reserved.
机译:松辽盆地南部长岭凹陷上白垩统青山口组是主要勘探目标之一。但是,尚未发现源岩沉积和原油的起源。对青山口组的十五种原油和二十二个烃源岩样品进行了岩石热解,气相色谱-质谱和碳同位素分析等综合地球化学研究,以提供对源有机质,沉积环境的新认识。对烃源岩样品的大量地球化学分析表明,青山口组的下段比中段具有更大的生烃潜力。这两个潜在的烃源岩组分被解释为沉积在略有不同的环境中,并且具有不同的由生物标志物组合确定的有机质来源。下半部富含有机物(平均TOC = 1.27 wt。%),易油,成熟且在缺氧条件下沉积,腐泥土有机物的贡献更大。中间构件有机物贫乏(平均TOC = 0.78 wt。%),易燃气体,较不成熟,并且在较少的缺氧条件下沉积,并且输入了更多的陆源有机质。生物标志物指纹图谱和碳同位素组成表明,所有原油都具有遗传相关性,可以归为一个油族,其中下层烃源岩贡献很大,而中层烃源岩贡献很小。 (C)2015 Elsevier Ltd.保留所有权利。

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