Origin and distribution model of the lower Paleozoic carbonate reservoirs in Pingfangwang-Pingnan buried hills, Dongying Sag

被引:0
|
作者
Cheng X. [1 ]
Cao Y. [1 ,2 ]
Yuan G. [1 ,2 ]
Wang Y. [1 ,2 ]
Zan N. [1 ]
机构
[1] Key Laboratory of Deep Oil and Gas in China University of Petroleum(East China), Qingdao
[2] Function Laboratory of Marine Geo-Resource Evaluation and Exploration Technology, Qingdao
来源
Cao, Yingchang (cyc8391680@163.com) | 1600年 / University of Petroleum, China卷 / 44期
关键词
Carbonate rocks; Distribution model; Origin of reservoirs; Pingfangwang-Pingnan buried hills; The lower Paleozoic;
D O I
10.3969/j.issn.1673-5005.2020.03.001
中图分类号
学科分类号
摘要
In view of the complexity of both the distribution and origin of the lower Paleozoic carbonate reservoirs in the Bohai Bay Basin as well as its importance to hydrocarbon exploration, the characters and origin of the lower Paleozoic carbonate reservoirs of Pingfangwang-Pingnan buried hills in Dongying Sag were studied using drilling cores and production data as well as a combination of conventional petrophysical property analysis, thin section analysis and element geochemistry. The distribution model of the reservoirs was established accordingly. The results show that the reservoirs are dominated by secondary pores, caves and fissures. The complex origin and distribution of the reservoirs resulted from a combination of several geological processes, such as epikarst, faulting and magma intrusion. The monadnock-type buried hills experienced two generations of epikarst which took place in the Caledonian and Indosinian-Yanshan stages, resulting in the pore-cave-fissure compound reservoirs at the top of the buried hills. Meanwhile, the magma intrusion at the lower part and accompanied dissolution led to pore-fissure type inner reservoirs. As for the fault block buried hills, the fracturing effect of fault or its combination with the Caledonian stage epikarst caused pore-cave-fissure compound reservoirs at the top of the buried hills. The lower part is characterized by induced joints caused by faults or magma intrusion with a small portion of dissolution, forming pore-fissure type inner reservoirs. © 2020, Editorial Office of Journal of China University of Petroleum(Edition of Natural Science). All right reserved.
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页码:1 / 14
页数:13
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