龙门山断裂带横断层成因类型及地质意义

王伟锋; 朱传华; 张晓杰; 卿艳彬; 单新建

doi:10.3799/dqkx.2016.062

Volume 41 Issue 5

May 2016

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Wang Weifeng, Zhu Chuanhua, Zhang Xiaojie, Qing Yanbin, Shan Xinjian, 2016. Genetic Types and Geological Significances of Transverse Faults at Longmenshan Fault Zone. Earth Science, 41(5): 729-741. doi: 10.3799/dqkx.2016.062

Citation:

Wang Weifeng, Zhu Chuanhua, Zhang Xiaojie, Qing Yanbin, Shan Xinjian, 2016. Genetic Types and Geological Significances of Transverse Faults at Longmenshan Fault Zone. Earth Science, 41(5): 729-741. doi: 10.3799/dqkx.2016.062

Citation:

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Genetic Types and Geological Significances of Transverse Faults at Longmenshan Fault Zone

doi: 10.3799/dqkx.2016.062

1.
School of Geosciences, China University of Petroleum, Qingdao 266580, China
2.
Bureau of Coal Geology of Hunan Province, Changsha 410014, China
3.
State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China

Received Date: 2015-11-06
Publish Date: 2016-05-15

Abstract

Abstract

Study on transverse faults in the Longmenshan fault zone is inadequate so far. Based on the regional geology, gravity data, magnetic data, distribution of earthquake and velocity data, combined with field study and structural modeling, the genetic types and geological significances of transverse faults at the Longmenshan fault zone were studied. It is found that: (1) There are 6 transverse faults in the northern and central Longmenshan fault zone, namely, the Bailongjiang, Nanba, Huya, Qingping, Xiaoyudong and Wolong-Huaiyuan transverse faults, where Huya fault is the boundary between the northern and central Longmenshan fault zones, while the Wolong-Huaiyuan fault is between the southern and central Longmenshan fault zone; (2) Transverse faults mainly have three genetic types, they are the transfer faults resulted from the reaction of the pre-existing NW-trending faults or weak belts and the nonsynchronous movement of the thrust faults, X-type conjugate shear faults and transverse extensional faults; (3) Transverse faults cut the Longmenshan fault zone into several segments and transfer the differences of the stratum, the geomorphology, the movement intensity, width of the thrust belts, earthquake intensity and frequency of different segments, besides, transverse faults could be independent seismogenic faults which may trigger earthquakes with the Longmenshan major fault belts and restrict the spread of aftershocks.
- Longmenshan fault zone,
- transverse fault type,
- characteristics of transverse fault,
- formation mechanism,
- tectonics

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References(92)

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Genetic Types and Geological Significances of Transverse Faults at Longmenshan Fault Zone

doi: 10.3799/dqkx.2016.062

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