鄂尔多斯盆地延长组泥页岩硅质来源与油气富集

刘国恒; 翟刚毅; 邹才能; 黄志龙; 夏响华; 石砥石; 周志; 陈榕; 张聪; 于抒放

doi:10.11781/sysydz201901045

鄂尔多斯盆地延长组泥页岩硅质来源与油气富集

doi: 10.11781/sysydz201901045

1. 中国地质调查局油气资源调查中心, 北京 100083;
2. 中国石油大学(北京) 油气资源与探测国家重点实验室, 北京 102200;
3. 中国石油勘探开发研究院, 北京 100083

基金项目:

国家科技重大专项项目（2016ZX05034-001）、国家重点研发计划政府间国际科技创新合作重点专项（2017YFE0106300）、国家自然科学基金项目（41272156）、中国地质调查项目（121201021000172121）和博士后基金项目（2018M641431）共同资助。

详细信息

作者简介:
刘国恒(1988-),男,博士后,从事油气藏形成与分布研究。E-mail:liuguoheng123@sina.cn。

通讯作者:
翟刚毅(1958-),男,教授级高级工程师,从事油气基础地质研究和战略选区调查。E-mail:zhaigangyi@126.com。

中图分类号: TE122.116
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出版历程
- 收稿日期: 2018-09-20
- 修回日期: 2018-12-03
- 刊出日期: 2019-01-28

Silicon sources and hydrocarbon accumulation in shale, Triassic Yanchang Formation, Ordos Basin

1. Oil and Gas Survey, China Geological Survey, Beijing 100083, China;
2. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102200, China;
3. Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China

摘要

摘要: 为了弄清鄂尔多斯盆地上三叠统延长组长7段和长9段泥页岩硅质来源与油气富集上的差异性，进行了主微量元素分析、全岩黏土X衍射、岩石热解、有机碳分析和扫描电镜观察研究。延长组泥页岩中长7²亚段和长9段在硅质来源、矿物组成、元素组成和有机地化特征方面表现出更多相似之处，而长7³亚段泥页岩与前面2套泥页岩则表现出一定的差异性。长7²亚段和长9段泥页岩中的硅质主要来自于陆源碎屑物质，而长7³亚段泥页岩硅质则表现出2种来源特征，即陆源碎屑来源和湖底热液喷流。延长组长7段和长9段泥页岩均是非常优质的烃源岩。但相比之下，受湖底热液作用的影响，长7³亚段泥页岩残留烃和干酪根含量更高，干酪根类型也更好，页岩油饱和度指数更高。因此，长7³亚段要优于长7²亚段和长9段泥页岩，具有更高的开采价值。
- 硅质来源 /
- 湖底热液 /
- 油气富集 /
- 延长组 /
- 三叠系 /
- 鄂尔多斯盆地
Abstract: A series of analyses, including major and trace element analysis, X-ray diffraction for bulk and clay mineral composition, Rock-Eval analysis, TOC analysis and scanning electron microscope observation, were conducted in order to determine the different silica sources and hydrocarbon accumulation between the Chang 7 member and Chang 9 member shale of the Triassic Yanchang Formation in the Ordos Basin. The Chang 7² sub-member and the Chang 9 member shale had more similarities in silica sources, mineral composition, element composition and organic geochemical characteristics, while the Chang 7³ sub-member shale showed certain differences in the above properties from the other two sets of shale reservoirs. The silica in the Chang 7² sub-member and the Chang 9 member shale came from terrestrial detritus, while the silica in the Chang 7³ sub-member shale showed the characteristics of two sources, namely, terrestrial detritus and hydrothermal from vents at the bottom of the lake. Both Chang 7 and Chang 9 shales are high-quality source rocks. However the contents of residual hydrocarbon and kerogen are higher, the type of kerogen is much better, and the oil saturation index is higher under the influence of hydrothermal fluid for the Chang 7³ sub-member shale. Hence the Chang 7³ sub-member is superior to the Chang 7² sub-member and Chang 9 member shale and has higher exploitation value.
- silica resource /
- hydrothermal fluid /
- hydrocarbon enrichment /
- Yanchang Formation /
- Triassic /
- Ordos Basin

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