阿尔金山各边界断裂的归属性

伍跃中; 李荣社; 王战; 雷学武; 张转; 谢丛瑞

Volume 32 Issue 5

Sep. 2007

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Article Navigation > Earth Science > 2007 > 32(5): 662-670

WU Yue-zhong, LI Rong-she, WANG Zhan, LEI Xue-wu, ZHANG Zhuan, XIE Cong-rui, 2007. The Attribution of Altyn Marginal Faults. Earth Science, 32(5): 662-670.

Citation:

WU Yue-zhong, LI Rong-she, WANG Zhan, LEI Xue-wu, ZHANG Zhuan, XIE Cong-rui, 2007. The Attribution of Altyn Marginal Faults. Earth Science, 32(5): 662-670.

WU Yue-zhong, LI Rong-she, WANG Zhan, LEI Xue-wu, ZHANG Zhuan, XIE Cong-rui, 2007. The Attribution of Altyn Marginal Faults. Earth Science, 32(5): 662-670.

Citation:

WU Yue-zhong, LI Rong-she, WANG Zhan, LEI Xue-wu, ZHANG Zhuan, XIE Cong-rui, 2007. The Attribution of Altyn Marginal Faults. Earth Science, 32(5): 662-670.

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The Attribution of Altyn Marginal Faults

1.
Xi′an Institute of Geology and Mineral Resources, Xi′an 710054, China
2.
Department of Geology, North west University, Xi′an 710069, China

Received Date: 2007-06-16
Publish Date: 2007-09-25

Abstract

Abstract

The South Altyn marginal fault, northwest Altyn border fault and Hongliugou-Lapeiquan fault in the northern edge of Altyn belong to different fault systems. The south marginal fault was formed in Proterozoic. In mid-late Paleozoic, it was a great intracontinental transform fault of right-lateral slip, and in Mesozoic and Neozoic it was revived in different parts. The northwest fault was formed later. Intense left-lateral slip occurred in Mesozoic-Neozoic and it belongs to the Asian slump fault system. Hongliugou-Lapeiquan fault zone belongs to the central tectonic system of Tarim block. It is an ophiolite complex belt and in early Palaeozoic it was the rift of continental or intercontinental margin. The three faults are different in the evolution history, movement form and tectonic significance, but they are interrelated and affect each other strongly. It is very important to study their tectonic attributions systematically for understanding the west tectonic framework of our country.
- Altyn,
- fault structure,
- fault evolvement,
- transform fault,
- conjugate slump fault system.

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References(68)

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