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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Occurrence and distribution of high molecular weight hydrocarbons in selected non-marine source rocks from the Liaohe, Qaidam and Tarim Basins, China
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Occurrence and distribution of high molecular weight hydrocarbons in selected non-marine source rocks from the Liaohe, Qaidam and Tarim Basins, China

机译:辽河,柴达木和塔里木盆地部分非海洋烃源岩中高分子量烃的赋存与分布

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摘要

Extracts of 18 potential source rocks from the Qaidam, Liaohe, and Tarim Basins, China have been characterized by high temperature gas chromatography (HTGC) and found to contain high molecular weight hydrocarbons (HMWHCs) above C-40. These rocks were originally formed in freshwater lacustrine, saline lacustrine, and terrigenous bog environments with mudstone, calcareous mudstone, coaly shale and coal lithologies. Their ages range from Triassic to Miocene and maturities from immature to mature covering a vitrinite reflectance range (R-o) for the Liaohe and Tarim samples of 0.54-0.84%. The combined distributions of the n-alkane and alkylcyclopentane homologues in the extracts can be used to characterize the nature of the original depositional environment. In certain samples the carbon number predominance of the n-alkanes changes from an odd/even predominance to even/odd predominance above C-40 possibly suggesting different precursors for the n-alkanes above and below C-40. Concentrations of the HMWHCs were also observed to increase with maturity of the source rocks. This is the first comprehensive report on the occurrence of HMWHCs in source rocks and their discovery introduces the possibility of using these compounds for oil/source rock correlation purposes in future studies along with the more conventional biomarkers. (C) 2003 Elsevier Ltd. All rights reserved. [References: 53]
机译:来自中国柴达木,辽河和塔里木盆地的18种潜在烃源岩的提取物已通过高温气相色谱(HTGC)进行了表征,发现含有C-40以上的高分子量碳氢化合物(HMWHCs)。这些岩石最初是在淡水湖相,盐湖相和泥质,钙质泥岩,煤质页岩和煤岩性的陆源沼泽环境中形成的。他们的年龄从三叠纪到中新世,成熟期从不成熟到成熟,覆盖辽河和塔里木样品的镜质体反射率范围(R-o)为0.54-0.84%。提取物中正构烷烃和烷基环戊烷同系物的组合分布可用于表征原始沉积环境的性质。在某些样品中,正构烷烃的碳数优势从C-40以上的奇数/偶数优势变为偶数/奇数优势,可能暗示了C-40之上和之下的正构烷烃的前体不同。还观察到HMWHCs的浓度随烃源岩的成熟而增加。这是有关烃源岩中HMWHCs发生的第一份综合报告,其发现引入了在未来的研究中将这些化合物与更常规的生物标志物一起用于油/烃源岩相关性的可能性。 (C)2003 Elsevier Ltd.保留所有权利。 [参考:53]

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