喜马拉雅运动对库车坳陷油气成藏的影响

曾联波; 周天伟; 吕修祥

Volume 27 Issue 6

Jun. 2002

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Article Navigation > Earth Science > 2002 > 27(6): 741-744

CENG Lian-bo, ZHOU Tian-wei, LÜ Xiu-xiang, 2002. Influence of Himalayan Orogeny on Oil & Gas Forming in Kuqa Depression, Tarim Basin. Earth Science, 27(6): 741-744.

Citation:

CENG Lian-bo, ZHOU Tian-wei, LÜ Xiu-xiang, 2002. Influence of Himalayan Orogeny on Oil & Gas Forming in Kuqa Depression, Tarim Basin. Earth Science, 27(6): 741-744.

CENG Lian-bo, ZHOU Tian-wei, LÜ Xiu-xiang, 2002. Influence of Himalayan Orogeny on Oil & Gas Forming in Kuqa Depression, Tarim Basin. Earth Science, 27(6): 741-744.

Citation:

CENG Lian-bo, ZHOU Tian-wei, LÜ Xiu-xiang, 2002. Influence of Himalayan Orogeny on Oil & Gas Forming in Kuqa Depression, Tarim Basin. Earth Science, 27(6): 741-744.

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Influence of Himalayan Orogeny on Oil & Gas Forming in Kuqa Depression, Tarim Basin

1.
Resources and Information Institute, University of Petroleum, Beijing 102249, China
2.
Key Laboratory for Hydrocarbon Accumulation, Ministry of Education, Beijing 102249, China

Received Date: 2002-08-12
Publish Date: 2002-11-25

Abstract

Abstract

Himalayan orogeny refers to the tectonic movement from Cenozoic, and it is the main power responsible for the formation of depressions and traps. Therefore, it plays an important role in oil and gas forming in Kuqa depression, Tarim basin. Rapid sedimentation and embedding by violent tectonic extrusion of Himalayan orogeny caused oil and gas to form. A lot of fractures formed by the orogeny are the main seepage and the valid storage space to improve the capability of low-permeability reservoir. Fault related with fold formed in the early Himalayan orogeny and ended in its late stage is the most favorable structural trap. Himalayan orogeny not only formed migration passage and accumulation location of oil and gas in Kuqa depression, but also was the main power for oil and gas migration. Meanwhile, it controlled oil and gas pool to be distributed in rows and zones. Faults and tectonic uplift in the late stage of Himalayan orogeny are the main factors on gas dissipating and the secondary oil and gas pool forming above salt layer in Eogene.
- Himalayan orogeny,
- oil and gas forming,
- Kuqa depression,
- Tarim basin

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References(6)

References

[1]	地质辞典编委会. 地质辞典(一): 普通地质———构造地质分册(下册)[M]. 北京: 地质出版社, 1983.395 Editorial Comittee of Geological Dictionary. Geological dictionary(Ⅰ): general geology— structural geology fascicule(the second volume)[M]. Beijing: Geological Publishing House, 1983. 395.
[2]	贾承造. 中国塔里木盆地构造特征与油气[M]. 北京: 石油工业出版社, 1997. JIA C Z. Structural characteristics and petroleum of Tarim basin, China[M]. Beijing: Petroleum Industry Press, 1997.
[3]	刘志宏, 卢华复, 贾承造, 等. 库车再生前陆逆冲带造山运动时间、断层滑移速率的厘定及其意义[J]. 石油勘探与开发, 2000, 27 (1): 12-15. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200001003.htm LIUZ H, LUHF, JIAC Z, et al. Orogeny timing and fault- slip rate and their significance to the rejuvenated foreland thrust belt of Kuche[J]. Petroleum Exploration and Development, 2000, 27(1): 12-15. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200001003.htm
[4]	刘志宏, 卢华复, 贾承造, 等. 库车再生前陆盆地的构造与油气[J]. 石油与天然气地质, 2001, 22 (4): 297-302. doi: 10.3321/j.issn:0253-9985.2001.04.003 LIUZ H, LUHF, JIA C Z, et al. Structures and hydrocarbon accumulation in Kuche rejuvenated foreland basin[J]. Oil&Gas Geology, 2001, 22 (4): 297-302. doi: 10.3321/j.issn:0253-9985.2001.04.003
[5]	秦胜飞, 贾承造, 陶士振. 塔里木盆地库车坳陷油气成藏的若干特征[J]. 中国地质, 2002, 29 (1): 103-108. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200201016.htm QIN S F, JIA C Z, TAO S Z. Some characteristics of oil and gas accumulation in the Kuche depression, Tarim basin[J]. Chinese Geology, 2002, 29 (1): 103-108. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200201016.htm
[6]	赵林, 秦胜飞. 库车坳陷天然气成藏条件分析[J]. 石油实验地质, 1999, 21 (4): 307-310. doi: 10.3969/j.issn.1001-6112.1999.04.005 ZHAO L, QINS F. Analysis on the pool-forming conditions of natural gas accumulations in the Kuche depression[J]. Experimental Petroleum Geology, 1999, 21 (4): 307-310. doi: 10.3969/j.issn.1001-6112.1999.04.005