塔里木盆地古城墟隆起奥陶系多期古流体活动证据及意义

鲁子野; 陈红汉; 丰勇; 吴悠; 熊万林; 尚培

doi:10.3799/dqkx.2015.137

Volume 40 Issue 9

Sep. 2015

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Article Navigation > Earth Science > 2015 > 40(9): 1529-1537

Lu Ziye, Chen Honghan, Feng Yong, Wu You, Xiong Wanlin, Shang Pei, 2015. Evidences of Multi-Episodically Paleo-Fluid Flow and Its Significance in Ordovician of Guchengxu Uplift, Tarim Basin. Earth Science, 40(9): 1529-1537. doi: 10.3799/dqkx.2015.137

Citation:

Lu Ziye, Chen Honghan, Feng Yong, Wu You, Xiong Wanlin, Shang Pei, 2015. Evidences of Multi-Episodically Paleo-Fluid Flow and Its Significance in Ordovician of Guchengxu Uplift, Tarim Basin. Earth Science, 40(9): 1529-1537. doi: 10.3799/dqkx.2015.137

Citation:

Lu Ziye, Chen Honghan, Feng Yong, Wu You, Xiong Wanlin, Shang Pei, 2015. Evidences of Multi-Episodically Paleo-Fluid Flow and Its Significance in Ordovician of Guchengxu Uplift, Tarim Basin. Earth Science, 40(9): 1529-1537. doi: 10.3799/dqkx.2015.137

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Evidences of Multi-Episodically Paleo-Fluid Flow and Its Significance in Ordovician of Guchengxu Uplift, Tarim Basin

doi: 10.3799/dqkx.2015.137

Lu Ziye^1
,,
Chen Honghan^{1, 2
,
,},
Feng Yong³,
Wu You³,
Xiong Wanlin⁴,
Shang Pei¹

1.
Key Laboratory of Tectonics and Petroleum Resources of the Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Lanzhou Center for Oil and Gas Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Lanzhou 730000, China
3.
College of Geoscience, Yangtze University, Jingzhou 434023, China
4.
China National Offshore Oil Corporation Limited-Shenzhen, Guangzhou 510240, China

Received Date: 2015-04-03
Publish Date: 2015-09-15

Abstract

Abstract

There is significant relationship among deep paleo-fluid flows and modification of carbonate reservoirs and hydrocarbon migration and accumulation. In this study, 11 samples of the Ordovician in Guchengxu uplift have been employed to make diagenetic observation and fluid inclusion measurement. The analyzed results indicate that there are three events of paleo-fluid flows in the Middle and Lower Ordovician of Guchengxu uplift. (1) The first event of paleo-fluid flows is represented by the first generation of calcite cement filling in high angle and meshy fractures. It is estimated that the calcite cement precipitated during late Caledonian tectonic movement. (2) The second event of paleo-fluid flows is represented by the second generation of hydrothermal dolomites. It is estimated that the saddle dolomite precipitated during the Permian volcanic activities. (3) The third event of paleo-fluid flows is represented by the third generation of calcite cement filling in the central residual spaces of the fractures and vugs. It records the gas accumulation during the later Himalayan. The bitumen distributed along the side of first generation calcite cement implies that the early charging oil accompanied with the first event of paleo-fluid flow had been damaged. The second event of paleo-fluid flow played a role of dolomitization which was in favor of the Ordovician reservoir improvement. The third event of paleo-fluid flow is associated with natural gas filling. It is concluded that the later Himalayan charging natural gases are the favorable exploration target in this area.
- Tarim basin,
- Guchengxu uplift,
- Ordovician,
- paleo-fluid flow,
- fluid inclusion,
- petroleum geology,
- stratigraphy

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References(58)

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