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The Research of Origin of Deep Natural Gas of Qianbei Sub-Sag in the south of Songliao Basin

机译:松辽盆地南北黔北凹陷深天然气起源研究

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This paper analyses the origins of deep natural gas in Qianbei Subsag using a variety of analytical data such as the natural gas components, the isotope and the light hydrocarbon analysis combining with the development characteristics of hydrocarbon source rocks. The study results show as the following: The abundance of organic matter from hydrocarbon source rocks in Qianbei Subsag is high and dominated by humus type. Part of good hydrocarbon source rocks of Type Ⅱ1 and Type Ⅱ2 are developed in Yingcheng Formation and these are the major gas source rocks that is in the stage of postmaturity in evolution degree. The natural gas component is dominated by methane and non-hydrocarbon gas content is low. The isotope values of ethane are lighter and methane and ethane have an obvious phenomenon of carbon isotopic reversal. Parent material types of methane and ethane are from different sources. The sources of methane are biased to humic parent material while the sources of ethane are biased to sapropelic parent material.
机译:本文分析了使用各种分析数据,如天然气组分,同位素和光源分析的各种分析数据分析了Qianbei Subsag的起源,与烃源岩的显影特性相结合。研究结果显示如下:黔北地位中烃源岩的丰富有机物高,由腐殖质型支配。 Ⅱ1型良好烃源岩体的一部分和Ⅱ2型型繁成形成,这些是在进化程度的后期阶段的主要气体源岩。天然气组分由甲烷和非烃类气体含量为主。乙烷的同位素值较轻,甲烷和乙烷具有明显的碳同位素逆转现象。母体材料类型的甲烷和乙烷来自不同的来源。甲烷的来源偏向于腐殖质母体材料,同时乙烷的来源偏向于Sapropelic母体材料。

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