韩国下白垩统晋州组焦沥青赋存状态

IF 0.3 Q4 GEOSCIENCES, MULTIDISCIPLINARY
T. Choi, H. Lim, Jae Il Lee, Y. Lee
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引用次数: 0

摘要

本研究首次报道了韩国庆尚盆地辛洞群白垩系金居砂岩中黑色不透明烃(焦沥青)的存在。焦沥青是在绿泥石孔隙衬水泥上形成的,或浸渍在绿泥石水泥的外部区域中。因此,它似乎是在绿泥石水泥沉淀后形成的,表明以前存在原油。液态烃在适度埋藏期间迁移到砂岩中,这些砂岩似乎起到了液态烃储层的作用。金聚组火山沥青的存在表明该组在液态烃运移后经历了深埋。随着储层温度的进一步升高,碳氢化合物被裂解,固体焦沥青残留物留在储层中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Occurrence of Pyrobitumen in the Lower Cretaceous Jinju Formation, Korea
: Occurrence of black opaque hydrocarbon (pyrobitumen) in some Cretaceous Jinju sandstones of the Sindong Group, Gyeongsang Basin in Korea is first reported in this study. The pyrobitumen is developed on chlorite pore-lining cement, or impregnated into the outer zone of chlorite cement. Therefore, it seems to have been formed after the precipitation of chlorite cement, indicating the former presence of crude oil. The liquid hydrocarbons migrated into sandstones during moderate burial and these sandstones seem to have acted as a liquid hydrocarbon reservoir. The presence of pyrobitumen in the Jinju Formation indicates that this formation underwent deep burial after liquid hydrocarbon migration. As reservoir temperatures increased further, hydrocarbons were cracked and a solid pyrobitumen residue remained in the reservoir.
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来源期刊
Journal of the Korean Earth Science Society
Journal of the Korean Earth Science Society GEOSCIENCES, MULTIDISCIPLINARY-
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50.00%
发文量
46
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