川东北地区飞仙关组台缘带鲕滩分布规律

刘建强; 罗冰; 谭秀成; 江兴福; 李宗银; 乔琳; 薛玖火; 赵长城

doi:10.3799/dqkx.2012.089

Volume 37 Issue 4

Jul. 2012

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Article Navigation > Earth Science > 2012 > 37(4): 805-814

LIU Jian-qiang, LUO Bing, TAN Xiu-cheng, JIANG Xing-fu, LI Zong-yin, QIAO Lin, XUE Jiu-huo, ZHAO Chang-cheng, 2012. Distribution of Marginal-Platform Oolitic Shoal in Feixianguan Formation, Northeast Sichuan, China. Earth Science, 37(4): 805-814. doi: 10.3799/dqkx.2012.089

Citation:

LIU Jian-qiang, LUO Bing, TAN Xiu-cheng, JIANG Xing-fu, LI Zong-yin, QIAO Lin, XUE Jiu-huo, ZHAO Chang-cheng, 2012. Distribution of Marginal-Platform Oolitic Shoal in Feixianguan Formation, Northeast Sichuan, China. Earth Science, 37(4): 805-814. doi: 10.3799/dqkx.2012.089

Citation:

LIU Jian-qiang, LUO Bing, TAN Xiu-cheng, JIANG Xing-fu, LI Zong-yin, QIAO Lin, XUE Jiu-huo, ZHAO Chang-cheng, 2012. Distribution of Marginal-Platform Oolitic Shoal in Feixianguan Formation, Northeast Sichuan, China. Earth Science, 37(4): 805-814. doi: 10.3799/dqkx.2012.089

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Distribution of Marginal-Platform Oolitic Shoal in Feixianguan Formation, Northeast Sichuan, China

doi: 10.3799/dqkx.2012.089

1.
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu 610500, China
2.
Research Institute of Petroleum Exploration and Development, Southwest Oil and Gas Field Company, PetroChina, Chengdu 610041, China
3.
School of Resources and Environment, Southwest Petroleum University, Chengdu 610500, China
4.
Exploration Division of PetroChina Southwest Oil and Gas Field Company, Chengdu 610041, China
5.
Geological Exploration and Development Research Institute, Chuanqing Drilling Engineering Co. Ltd. of CNPC, Chengdu, China 610051

Received Date: 2012-02-07
Available Online: 2021-10-13
Publish Date: 2012-07-15

Abstract

Abstract

To better probe the laws of distribution of oolitic shoal which lies in the platform margin of Feixianguan Formation, Sichuan basin to facilitate the exploration and development on the oolitic shoal gas pool, this paper analyses the development properties and distribution law of platform margin shoal by means of case study of northeastern region of Sichuan basin, after which it points out that this type of oolitic shoal expands in the direction of NW-SE along the platform margin and stretches in "finger-shape" to the platform interior from which two groups of positive faults basement cross in directions of NE and NW, while the extension direction of the "finger-shape" is vertical to the platform margin. Furthermore, paleogeography framework formed by syndepositional activities of basement cracking, sedimentary paleogeomorphology and relative sea level change dominates the longitudinal and horizontal discipline of this oolitic shoal jointly. First, syndepositional tension of basement cracking in the direction NW contributes to the sedimentary framework of platform-hollow differentiation, which simultaneously controls the distribution of platform margin and also facies of oolitic shoal on it., while that of NE one aggravates the degree of differentiation of sedimentary geomorphy in the researching area. Oolitic shoal of platform margin occurs on the "cracking uplift" highland formed by the basement cracking in the direction of NE-SW, which migrates to the internal platform, characterized by the fault controlling oolitic shoal of platform margin fingered slim zone of "belts dominated by NW, decorated by NE". Second, the relative eustasy regulates sedimentary thickness and scale. Consequently an integration model of multi-factor on the shoal of platform margin can be established eventually.
- basement cracking,
- oolitic shoal,
- platform margin,
- Feixianguan Formation,
- Northeast Sichuan,
- sedimentology,
- petroleum reservoirs

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Distribution of Marginal-Platform Oolitic Shoal in Feixianguan Formation, Northeast Sichuan, China

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