首页> 外文期刊>Petroleum Science and Technology >Geochemical characteristics of Chang 9(1)source rocks of upper Triassic Yanchang formation in Zhidan-Ansai area, Ordos Basin and its significance for tight oil exploration
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Geochemical characteristics of Chang 9(1)source rocks of upper Triassic Yanchang formation in Zhidan-Ansai area, Ordos Basin and its significance for tight oil exploration

机译:鄂尔多斯盆地鄂尔多斯盆地中三叠纪盐昌地区昌9(1)源岩的地球化学特征及其对严格石油勘探的重要性

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摘要

The average total organic carbon (TOC) content of Chang 9(1)source rocks is 4.85%, and the main kerogen type is II1, and the average pyrolysis peak temperature is 452 degrees C in Zhidan-Ansai area, Ordos Basin. These show that Chang 9(1)source rocks have reached good to excellent level and peak hydrocarbon generation stage. Chang 9(1)source rocks were formed in semi-deep lacustrine sedimentary environments of fresh-brackish water and weak oxidation-reduction. The discovery of Chang 9(1)source rock extends the oil exploration field of Yanchang Formation, especially in Zhidan area, it is a favorable area for further exploration in Chang 9 reservoir.
机译:鄂尔多斯盆地志丹-安塞地区长9(1)烃源岩的平均总有机碳(TOC)含量为4.85%,主要干酪根类型为II1,平均热解峰值温度为452℃。这表明长9(1)烃源岩已达到良好至良好水平和生烃高峰期。长9(1)烃源岩形成于淡水微咸水和弱氧化还原的半深湖相沉积环境。长9(1)烃源岩的发现拓展了延长组的勘探领域,尤其是志丹地区,是长9储层进一步勘探的有利地区。

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