| 南黄海海相中—古生界碳酸盐岩储层特征及成藏模式——对比四川盆地和苏北盆地 |
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| 引用本文： | 吴淑玉, 陈建文, 梁杰, 刘俊, 张银国, 袁勇. 南黄海海相中—古生界碳酸盐岩储层特征及成藏模式——对比四川盆地和苏北盆地[J]. 海洋地质前沿, 2016, 32(1): 13-21. doi: 10.16028/j.1009-2722.2016.01003 |
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| 作者姓名： | 吴淑玉 陈建文 梁杰 刘俊 张银国 袁勇 |
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| 作者单位： | 1 国土资源部海洋油气资源与环境地质重点实验室, 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, 青岛 266071;; 3 中国地质调查局青岛海洋地质研究所, 青岛 266071;; 4 中国地质大学(武汉)资源学院, 武汉 430074 |
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| 基金项目： | 国家海洋局海底重点实验室基金(KLSG1102) 中国地质调查局项目(GZH200800503) 国土资源部海洋油气资源和环境地质重点实验室基金(MRE201318,MRE201115) |
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| 摘 要： | 通过对比四川盆地、苏北盆地和南黄海盆地的钻井、测井、岩心、野外露头等资料,分析了南黄海中—古生界海相碳酸盐岩储层类型及其成藏模式。研究区存在白云岩孔隙储层、礁滩相储层、风化壳储层和裂隙储层,成藏模式有威远式、安岳式、五百梯式和普光式,并且预测南黄海崂山隆起具备以上4种成藏模式,为目前及将来勘探的重点目标。
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| 关 键 词： | 南黄海 海相中—古生界 碳酸盐岩 储层 成藏模式 |
| 收稿时间： | 2015-11-25 |
CHARACTERISTICS OF MESOZOIC-PALAEOZOIC MARINE CARBONATE RESERVOIR IN THE SOUTH YELLOW SEA BASIN AND HYDROCARBON ACCUMULATION:COMPARISON BETWEEN THE SICHUAN BASIN AND THE SUBEI BASIN |
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| WU Shuyu, LIANG Jie, LIANG Jie, LIU Jun, ZHANG Yinguo, YUAN Yong. CHARACTERISTICS OF MESOZOIC-PALAEOZOIC MARINE CARBONATE RESERVOIR IN THE SOUTH YELLOW SEA BASIN AND HYDROCARBON ACCUMULATION:COMPARISON BETWEEN THE SICHUAN BASIN AND THE SUBEI BASIN[J]. Marine Geology Frontiers, 2016, 32(1): 13-21. doi: 10.16028/j.1009-2722.2016.01003 |
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| Authors: | WU Shuyu LIANG Jie LIANG Jie LIU Jun ZHANG Yinguo YUAN Yong |
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| Affiliation: | 1 Key Laboratory of Marine Hydrocarbon Resources and Environment Geology, Ministry of Land and Resource, Qingdao 266071, China,;; 2 Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061, China,;; 3 Qingdao Institute of Marine Geology, CGS, Qingdao 266071, China;; 4 Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China |
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| Abstract: | Comparison of drilling, logging, core and outcrop data is made for the Mesozoic and Paleozoic carbonate reservoir in the Sichuan Basin, Subei Basin and the South Yellow Sea Basin, in order to reveal the similarities and differences of hydrocarbon accumulation in these basins. There are four kinds of reservoirs in this region, i.e. the porous dolomitic reservoir, reef-bank reservoir, weathering crust reservoir and fractured reservoir, and four kinds of hydrocarbon accumulation, namely the Weiyuan type, the Anyue type, the Wubaiti type and the Puguang type. It is predicted that the four types of hydrocarbon accumulation may all occur on the Laoshan Uplift of the South Yellow Sea Basin. |
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| Keywords: | South Yellow Sea Basin marine Mesozoic-Palaeozoic carbonatite reservoir hydrocarbon accumulation |
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