四川盆地元坝-通南巴地区关键构造期构造特征及陆相致密砂岩天然气成藏响应

刘昭茜; 罗开平; 唐永; 杨帆; 梅廉夫; 沈传波

doi:10.3799/dqkx.2019.032

Volume 44 Issue 3

Mar. 2019

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Article Navigation > Earth Science > 2019 > 44(3): 756-772

Liu Zhaoqian, Luo Kaiping, Tang Yong, Yang Fan, Mei Lianfu, Shen Chuanbo, 2019. Critical Tectonic Periods and the Response of Gas Accumulation in Non-Marine Tight Sandstone Reservoir in Yuanba-Tongnanba Area, Sichuan Basin. Earth Science, 44(3): 756-772. doi: 10.3799/dqkx.2019.032

Citation:

Liu Zhaoqian, Luo Kaiping, Tang Yong, Yang Fan, Mei Lianfu, Shen Chuanbo, 2019. Critical Tectonic Periods and the Response of Gas Accumulation in Non-Marine Tight Sandstone Reservoir in Yuanba-Tongnanba Area, Sichuan Basin. Earth Science, 44(3): 756-772. doi: 10.3799/dqkx.2019.032

Citation:

Liu Zhaoqian, Luo Kaiping, Tang Yong, Yang Fan, Mei Lianfu, Shen Chuanbo, 2019. Critical Tectonic Periods and the Response of Gas Accumulation in Non-Marine Tight Sandstone Reservoir in Yuanba-Tongnanba Area, Sichuan Basin. Earth Science, 44(3): 756-772. doi: 10.3799/dqkx.2019.032

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Critical Tectonic Periods and the Response of Gas Accumulation in Non-Marine Tight Sandstone Reservoir in Yuanba-Tongnanba Area, Sichuan Basin

doi: 10.3799/dqkx.2019.032

1.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Wuxi Research Institute of Petroleum Geology, SINOPEC Petroleum Exploration and Production Research Institute, Wuxi 214126, China
3.
School of Geosciences, Yangtze University, Wuhan 430100, China

Received Date: 2019-02-26
Publish Date: 2019-03-15

Abstract

Abstract

Most of the non-marine tight sandstone strata in the polycyclic superimposed basins in China is rich in hydrocarbon resources and exhibits complicated and specific hydrocarbon geological characteristics.Yuanba-Tongnanba area is located in a polycyclic and multi-attribute tectonic intersection.It is a typical region which could reveal the respond relationship between multiphase tectonization and non-marine tight gas accumulation in the polycyclic superimposed basin.Based on the seismic data, apatite fission track (AFT) geochronology and hydrocarbon accumulation characterizes analysis, two critical tectonic periods have been identified which are the Late Yanshan epoch (Late Cretaceous about 100-70 Ma) and the Early Himalayan epoch (Eocene to Olgocene about 40-25 Ma).The gas accumulation in the non-marine tight sandstone reservoirs was controlled by the tectonization of two critical tectonic periods.NE-trending structures were built in the Late Yanshan epoch which is the critical hydrocarbon accumulation period of NE-trending weak deformation zone, NW-SN trending transitional deformation belt (the west area of Tongnanba block) and NW-trending concentrated deformation belt.The respond pattern of Late Yanshan epoch could be expressed as earlier accumulation, terrestrial source, anticline control response on gas trap and fold control response on fractures.NW-trending and nearly SN-trending structures were built in the Early Himalayan epoch which is not only the critical hydrocarbon accumulation period of SN-trending transitional deformation belt and NW-SN trending transitional deformation belt (the east area of Yuanba block), but also the critical hydrocarbon reconstruction period of NW-SN trending transitional deformation belt (the west area of Tongnanba block) and NW-trending concentrated deformation belt.The respond pattern of Himalayan epoch could be expressed as late accumulation, marine-terrestrial mixed source, fault control response on gas trap and fault control response on fractures.
- Yuanba-Tongnanba area,
- critical tectonic period,
- tight sandstone gas,
- hydrocarbon accumulation response to tectonism,
- petroleum geology

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References(60)

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Critical Tectonic Periods and the Response of Gas Accumulation in Non-Marine Tight Sandstone Reservoir in Yuanba-Tongnanba Area, Sichuan Basin

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