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Discovery of Carboniferous Oil Seepage in Qaidam Basin and Its Geological Significance

机译:柴达木盆地石炭系石油渗漏的发现及其地质意义

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摘要

In this work, the oil seepage was found in calcite veins in Keluke formation of upper Carboniferous reservoirs. Based on the analysis of geochemical characteristics, the isomerization parameter of C-29 sterane 20S/(20S + 20R) was obtained as 0.39 and Ts/Tm value as 1.12, indicating that the oil seepage was mature. The Pr/Ph value was 0.64 and the tricyclic terpane was characterized by high abundance of gamacerane, C-27 > C-29 sterane, and a normal distribution with C-23 as the dominant peak. Moreover, the oil/oil and oil/source rock correlation of oil seepage and carboniferous source rock underground and surface indicated that the oil seepage was similar to crude in Mabei-2 well (1463m) and Sin-3 well (1076m) but was different from the other crude in north Qaidam basin. It is inferred that the oil seepage was authigenic crude in Carboniferous, and Carboniferous source rocks have contributed to the oils in Mabei-2 well (1463m) and Sin-3 well (1076m). This study offers new scientific evidence for the exploring of carboniferous in Qiandam basin.
机译:在这项工作中,在上石炭统储层的Keluke地层的方解石脉中发现了渗油现象。通过对地球化学特征的分析,得出C-29甾烷20S /(20S + 20R)的异构化参数为0.39,Ts / Tm值为1.12,表明渗油成熟。 Pr / Ph值为0.64,并且三环萜烯的特征是gamacerane的丰度很高,C-27> C-29甾烷,并且以C-23为主导峰呈正态分布。此外,地下渗油与石炭系烃源岩地下和地表的油/油和油/源岩相关性表明,马北2井(1463m)和新三井(1076m)的原油渗流与原油相似。来自柴达木盆地北部的其他原油。可以认为,石炭系的渗油是自生原油,石炭系烃源岩对马北二井(1463m)和辛三井(1076m)的油有贡献。该研究为前潭盆地石炭系的勘探提供了新的科学依据。

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