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Carbon isotope and origin of the hydrocarbon gases in the Junggar Basin, China

机译:准gar尔盆地的碳同位素与烃类气体的成因

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The genetic type, source and distribution of hydrocarbon gases in the Junggar Basin were clarified through the carbon isotope analysis. Mature to post mature oil-type gas, mature to post mature coal-type gas, transition gas and biogas are identified in the Junggar Basin. Partly reversed order of carbon isotope of hydrocarbon gases in the Junggar Basin are attributed to one or several of the following reasons: mixing of oil-type and coal-type gases, mixing of coal-type gases of different source, mixing of coal-type gases of varied maturity, and microbial action. Three types of coal-type gases in the Junggar Basin are identified. The first type of coal-type gases characterized with high δ13C values of heavy hydrocarbon gases (δ13C2>?26.0‰) are the mature to high mature gases that are generated from Jurassic source rocks. The second type of coal-type gases characterized with low δ13C values of heavy hydrocarbon gases (δ13C2
机译:通过碳同位素分析,明确了准gar尔盆地油气的成因类型,来源和分布。在准gar尔盆地发现了成熟到成熟的石油型天然气,成熟到成熟的煤型天然气,过渡气和沼气。准gar尔盆地烃类气体碳同位素的部分颠倒顺序归因于以下一种或几种原因:混合石油类和煤类气体,混合不同来源的煤类气体,混合煤类各种成熟气体和微生物作用。确定了准gar尔盆地的三种煤型气体。特征为重烃气体的δ13C值高(δ13C2>?26.0‰)的第一类煤系气体是由侏罗系烃源岩产生的成熟至高度成熟的气体。第二类煤系气体的特征是重烃气的δ13C值低(δ13C2<?26.0‰),成熟度范围大,是由二叠系侏罗纪,乌尔河和贾木河组的一个或几个烃源岩产生的。从石炭系烃源岩中产生的第三类煤系气体,其重烃气体的δ13C值宽且后期成熟度高。

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