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    Volume 44 Issue 3
    Mar.  2019
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    Article Contents
    Li Le, Wang Zixiang, Zheng Youheng, Chen Fengling, Wu Shiqiang, Qi Zhixian, Liu Aiwu, 2019. Mechanism of Shale Oil Enrichment from the Salt Cyclotherm in Qian3 Member of Qianjiang Sag, Jianghan Basin. Earth Science, 44(3): 1012-1023. doi: 10.3799/dqkx.2018.389
    Citation: Li Le, Wang Zixiang, Zheng Youheng, Chen Fengling, Wu Shiqiang, Qi Zhixian, Liu Aiwu, 2019. Mechanism of Shale Oil Enrichment from the Salt Cyclotherm in Qian3 Member of Qianjiang Sag, Jianghan Basin. Earth Science, 44(3): 1012-1023. doi: 10.3799/dqkx.2018.389

    Mechanism of Shale Oil Enrichment from the Salt Cyclotherm in Qian3 Member of Qianjiang Sag, Jianghan Basin

    doi: 10.3799/dqkx.2018.389
    • Received Date: 2018-12-10
    • Publish Date: 2019-03-15
    • Research on the shale oil enrichment mechanism of Qianjiang Formation is lacking.The data of core image, rock pyrolysis, vitrinite reflectance, biomarkers, maceral composition, rock petrophysics, well logging, and XPT well test were used to analyze the quality of source rock, reservoir property, and preservation condition in this study.The kerogens are predominantly type Ⅰ-Ⅱ1.The vitrinite reflectance ranges from 0.51% to 0.80%.The maturity indicators of C29 sterane in the rocks from the 10th cyclotherm in the Wangchang are obviously different from that of the underlying halite, which indicates that there are migrated oil.The porosity of the reservoir ranges from 7.8% to 26.3%.The halite layers are thick enough (> 6 m) and stable throughout the area distribution; moreover, they did not break during the stage of deposition and burial.With the excellent preservation condition and storage capacity, the hydrocarbon generated from the deeper source rocks within the 10th cyclotherm controlled the shale oil enrichment in higher structural position, while hydrocarbon generated in-situ dominated in the lower structural position.

       

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