海陆对比看南黄海海相中-古生界的生储盖组合特征

袁勇; 陈建文; 梁杰; 张鹏辉

doi:10.11781/sysydz201702195

海陆对比看南黄海海相中-古生界的生储盖组合特征

doi: 10.11781/sysydz201702195

袁勇^1,2,
陈建文^1,2, ,,
梁杰^1,2,
张鹏辉^1,2

1.
国土资源部海洋油气资源与环境地质重点实验室, 青岛海洋地质研究所, 山东青岛 266071
2. 海洋国家实验室海洋矿产资源评价与探测技术功能实验室, 山东青岛 266071

基金项目: 国土资源部项目（XQ-2005-01，2009GYXQ10）；中国地质调查局项目（GZH200800503，121201005000150008）和山东省博士后创新基金"南黄海盆地二叠系上统相震约束储层表征研究"（201602004）资助。

详细信息

作者简介:
袁勇(1988-),男,博士后,从事地质综合解释及油气地质学研究。E-mail:yuany010@126.com。

通讯作者:
陈建文(1965-),男,博士,研究员,从事海域油气资源调查评价与研究。E-mail:jwchen2012@126.com。

中图分类号: TE122
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出版历程
- 收稿日期: 2016-10-27
- 修回日期: 2017-02-10
- 刊出日期: 2017-03-28

Source-reservoir-seal assemblage of marine Mesozoic-Paleozoic in South Yellow Sea Basin by land-ocean comparison

Yuan Yong^1,2,
Chen Jianwen^{1,2
, ,},
Liang Jie^1,2,
Zhang Penghui^1,2

1.
Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology of Ministry of Land and Resources, Qingdao Institute of Marine Geology, Qingdao, Shandong 266071, China
2. Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao, Shandong 266071, China

摘要

摘要: 作为下扬子主体的南黄海盆地发育分布广泛、厚度大且较全的中-古生代海相地层，通过对比扬子陆域的烃源岩、储层及盖层特征，结合南黄海盆地近几年采集的地震剖面、钻井资料以及陆上野外露头资料，总结和分析了南黄海海相中-古生界的生储盖组合特征。南黄海海相地层发育下寒武统荷塘组/幕府山组、下志留统高家边组、下二叠统栖霞组和二叠系龙潭-大隆组4套烃源岩，对比扬子区陆域烃源岩特征，确定为较好的烃源岩。苏北-南黄海盆地储集层以碳酸盐岩为主，发育白云岩孔隙储层、礁滩相储层、风化壳储层和裂隙储层4种类型。研究认为南黄海发育扬子陆区已发现的典型油气藏的成藏层位，海相地层发育3套区域性的盖层和3套完整的生储盖组合，具有很好的油气远景。
- 生储盖组合特征 /
- 海相中-古生界 /
- 南黄海盆地 /
- 扬子区
Abstract: The South Yellow Sea Basin is the main body of the Lower Yangtze area, where marine Mesozoic-Paleozoic strata are widely distributed. The characteristics of source-reservoir-seal assemblage of the marine Mesozoic-Paleozoic strata in the South Yellow Sea Basin were analyzed by comparing the characteristics of hydrocarbon source rocks, reservoir and cap rocks, and combining with seismic sections, drilling and outcrop data. Four sets of hydrocarbon source rocks developed, including the Lower Cambrian Hetang and Mufushan formations, the Lower Silurian Gaojiabian Formation, the Lower Permian Qixia Formation, and the Upper Permian Longtan and Dalong formations. By comparing the characteristics of hydrocarbon source rocks of the Yangtze land area, the source rocks of the South Yellow Sea Basin may be classed as good hydrocarbon source rocks. Carbonate is the main reservoir type in the South Yellow Sea area, and there are four carbonate reservoir types: porous dolomitic, reef-bank, weathered crust and fractured. The marine strata of South Yellow Sea Basin developed three sets of regional cap rocks and three sets of complete assemblages. The South Yellow Sea Basin has very good oil and gas prospects.
- source-reservoir-seal assemblage /
- marine Mesozoic-Paleozoic /
- South Yellow Sea Basin /
- Yangtze block

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