柯坪地区中下寒武统走滑断裂带方解石脉期次、古流体演化与油气充注历史

刘建章; 陈诚; 蔡忠贤; 李杰; 吴正洲

doi:10.3799/dqkx.2023.089

Volume 48 Issue 6

Jun. 2023

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Article Navigation > Earth Science > 2023 > 48(6): 2189-2203

Liu Jianzhang, Chen Cheng, Cai Zhongxian, Li Jie, Wu Zhengzhou, 2023. Division of Calcite Veins Stage, Paleo-Fluid Evolution and Hydrocarbon Charging History in the Middle and Lower Cambrin Strike-Slip Fault Zone in Keping Area, Northwest of Tarim Basin. Earth Science, 48(6): 2189-2203. doi: 10.3799/dqkx.2023.089

Citation:

Liu Jianzhang, Chen Cheng, Cai Zhongxian, Li Jie, Wu Zhengzhou, 2023. Division of Calcite Veins Stage, Paleo-Fluid Evolution and Hydrocarbon Charging History in the Middle and Lower Cambrin Strike-Slip Fault Zone in Keping Area, Northwest of Tarim Basin. Earth Science, 48(6): 2189-2203. doi: 10.3799/dqkx.2023.089

Citation:

Liu Jianzhang, Chen Cheng, Cai Zhongxian, Li Jie, Wu Zhengzhou, 2023. Division of Calcite Veins Stage, Paleo-Fluid Evolution and Hydrocarbon Charging History in the Middle and Lower Cambrin Strike-Slip Fault Zone in Keping Area, Northwest of Tarim Basin. Earth Science, 48(6): 2189-2203. doi: 10.3799/dqkx.2023.089

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Division of Calcite Veins Stage, Paleo-Fluid Evolution and Hydrocarbon Charging History in the Middle and Lower Cambrin Strike-Slip Fault Zone in Keping Area, Northwest of Tarim Basin

doi: 10.3799/dqkx.2023.089

Liu Jianzhang^{1, 2
,
,},
Chen Cheng^{1, 2},
Cai Zhongxian^{1, 2
,
,},
Li Jie^{1, 2},
Wu Zhengzhou^{1, 3}

1.
Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
3.
The No.1 Gas Production Plant, Jianghan Oilfield Branch Company, SINOPEC, Chongqing 404120, China

Received Date: 2022-10-26
Publish Date: 2023-06-25

Abstract

Abstract

Multi-stage calcite veins and solid bitumen filled in the Middle and Lower Cambrian strike-slip fault zone of the field outcrops for Keping Area, northwest of Tarim basin, are important medium to reveal the fluid activity history and hydrocarbon accumulation process. Based on the observation of the filling and distribution characteristics of calcite veins and bitumen in outcrop of strike-slip fault zones, the paragenetic sequence of calcite veins and bitumen and the origin fluid properties were determined using the thin section observation, cathodoluminescence, in-situ trace and rare earth element testing, carbon and oxygen isotopes measurement, system analysis of fluid inclusion, and the evolution of paleo-fluid in the strike-slip fault zones of the Middle and Lower Cambrian and its coupling relationship with hydrocarbon charging process were investigated. The results show that there are at least five phases of calcite veins in the strike-slip fault zones of the Middle and Lower Cambrian for Keping area of Xinjiang, C1, C2, C3, C4 and C5 respectively. The C1 calcite vein-forming fluid was mainly derived from formation water of the local layer and partly mixed with the brine of the Awatage Formation that infiltrated along the strike-slip fault. The C2 and C3 calcite vein-forming fluids were mainly the mixture of formation water and hydrocarbon-bearing hydrothermal fluids, but the formation temperature of C3 was slightly lower. The C4 calcite vein-forming fluid was mainly formation water, and there was mixing of atmospheric fresh water. The C5 calcite vein-forming fluid was mainly the mixture of formation water, hydrocarbon-bearing hydrothermal fluid and atmospheric fresh water. The formation stages of C1, C2, C3, C4 and C5 calcite veins were associated with tectonic activities of Keping area and generated in the Middle and Late Caledonian periods, Middle and Late Hercynian periods, Indosinian to Middle Yanshanian periods, Late Yanshanian and Himalayan periods, respectively. Three hydrocarbon charging phases were recognized, the Middle and Late Hercynian periods, Indosinian to Middle Yanshanian period and Himalayan period, respectively. The Middle and Late Hercynian periods and the Middle Inindo-Yanshanian period may be the main formation period of the primary oil and gas reservoirs for the Middle and Lower Cambrian in the Keping area, and the Himalayan period was an important period of oil and gas reservoir adjustment and hydrocarbon reaccumulation. The traps formed in Himalayan period and related to strike-slip faults also have favorable conditions for petroleum accumulation.
- hydrocarbon charging history,
- paleo-fluid evolution,
- calcite vein,
- strike-slip fault zone,
- Keping area,
- petroleum geology

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References(63)

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Division of Calcite Veins Stage, Paleo-Fluid Evolution and Hydrocarbon Charging History in the Middle and Lower Cambrin Strike-Slip Fault Zone in Keping Area, Northwest of Tarim Basin

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