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Geochemical Characteristics of Crude Oils from Zao-V Oil Measures in Shenjiapu Oilfield

机译:沉家堡油田枣五井区原油地球化学特征

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摘要

The geochemical characteristics of crude oils from Zao- V oil measures in the Shenjiapu oilfield are systematically described in terms of the fractional composition of crude oils, GC characteristics of saturated hydrocarbon fraction of crude oils and the characteristics of their bio-markers. The depositional environment, type and evolution of the biological source are also discussed. All pieces of evidence such as low saturated hydrocarbon fraction, high resin and asphalt , high isoprenoid alkane, weak odd-carbon number predominance (CPI ranging from 1.23 to 1.29, OEP ranging from 1. 14 to 1.16) and low sterane and terpane maturity parameters show these crude oils are immature oils. Low Pr/Ph ratios (0.66 -0.88) and high gammacer-ance/C_(31) hopane ratios (0.59 -0. 86) indicate the source rocks were formed in a slightly saline to brackish reducing lake depositional environment. Gas chromatographic characteristics cf the saturated hydrocarbon fraction and the predominance of C_(30) hopane in terpane series and C_(29) sterane in sterane series indicate the biological source of the crude oils is composed mainly of bacterial and algal organic matter, and some algae are perhaps the main contributor of organic matter to the source rocks.
机译:从原油的成分组成,原油的饱和烃馏分的GC特征及其生物标志物的特征出发,系统地描述了沉家堡油田枣V井段原油的地球化学特征。还讨论了沉积环境,生物源的类型和演化。所有证据表明,例如低饱和烃馏分,高树脂和沥青,高类异戊二烯烷烃,弱奇碳数优势(CPI范围为1.23至1.29,OEP范围为1.14至1.16)以及低甾烷和萜烯成熟度参数表明这些原油是不成熟的油。低的Pr / Ph比(0.66 -0.88)和高的γ-钙化剂/ C_(31)ane烷比(0.59 -0。86)表示烃源岩是在微咸至微咸的湖泊沉积环境中形成的。气相色谱图谱的特征是饱和烃馏分和萜烯系列中的C_(30)hop烷和甾烷系列中的C_(29)甾烷占优势,表明原油的生物学来源主要由细菌和藻类有机物以及一些藻类组成可能是有机质对烃源岩的主要贡献者。

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