蒸发岩
地质学
成熟度(心理)
碳氢化合物
地球化学
生物标志物
有机质
烃源岩
有机地球化学
沉积岩
矿物学
构造盆地
化学
地貌学
有机化学
发展心理学
生物化学
心理学
出处
期刊:Advanced Materials Research
[Trans Tech Publications]
日期:2012-12-01
卷期号:616-618: 1042-1047
被引量:2
标识
DOI:10.4028/www.scientific.net/amr.616-618.1042
摘要
To investigate hydrocarbon potential of the evaporites, some deep wells such as Haoke-1 well and Fengshen-2 well were intensively cored, tested by TOC, Rock-Eval, and chromatography and mass spectrometry and evaluated using geochemistry of biomarker and hydrocarbon generation. High content of gammacerane and low Pr/Ph was exhibited in the evaporite system compared to the non-evaporite system. Different response of biomarkers parameters for the different sedimentary systems was exhibited, such as C19/(C19+C23) terpanes, C29/(C27+C28+C29) steranes, C24/C23 and C22/C21 tricyclic terpane. The evaporites and mud stones have the capacity to generate and expel hydrocarbons. The tested samples were mostly typeⅠand typeⅡ1 of organic matter, and their original generating capacity can reach 40 mg/g rock and 20 mg/g rock respectively. The efficiency of hydrocarbon expulsion reached 60%, but the distribution of organic matter and its generative potential was highly variable. In general, the mudstones show greater generative potential than the evaporites. High maturity severely reduced the capacity of their rocks to generate and expel petroleum.
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