青海天峻坳陷三叠系大加连组烃源岩特征
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The hydrocarbon source evaluation in Tianjun Triassic Depression of the South of Qilian Basin
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    摘要:

    天峻凹陷隶属于青海地区南祁连盆地,盆地三叠系广泛发育碳酸盐岩,且厚度较大。本文对天峻凹陷中三叠统大加连组烃源岩,进行采集样品,并对其地球化学特征进行分析。文章从有机质丰度、有机质类型和有机质成熟度等参数对天峻坳陷三叠系大加连组的海相烃源岩进行了评价。最后发现,烃源岩属于海相碳酸盐岩类已达到了烃源岩评价标准,其有机质丰度高,有机质类型普遍为Ⅱ2,有机质成熟度进入油气生成的成熟-高成熟期。但鉴于样品采集来自地表,考虑到演化作用和风化作用,天峻坳陷的中三叠统大加连组碳酸盐岩判定为中等烃源岩。

    Abstract:

    In the Tianjun region of the south Qilian basin,Marine carbonate has widely developed Middle Triassic calc-alkalic,which has a bigger thickness.According to the experiment and collect hydrocarbon source rocks data,we do some research in organic matter abundance,organic matter types and maturity of organic matter.In our opinion,the marine oil belongs to effective source beds.Organic matter abundance is high.And organic type belongs to Ⅱ2.Organic matter maturities of oil and gas have entered into the mature-high maturity period.Finally,we can conclude that the hydrocarbon source rocks of Tianjun region belongs to a middle grading considering of the effect of evolution function and weathering because the sample was collected from the ground surface.

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许睿,谭富荣.青海天峻坳陷三叠系大加连组烃源岩特征[J].河北工程大学自然版,2011,28(4):65-68

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  • 收稿日期:2011-08-29
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  • 在线发布日期: 2015-01-12
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