滇西北程海—宾川断裂带第四纪分段活动性的构造地貌表现与限定

黄小巾; 吴中海; 黄小龙; 罗睿洁

doi:10.3799/dqkx.2017.548

Volume 43 Issue 12

Dec. 2018

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Article Navigation > Earth Science > 2018 > 43(12): 4651-4670

Huang Xiaojin, Wu Zhonghai, Huang Xiaolong, Luo Ruijie, 2018. Tectonic Geomorphology Constrains on Quaternary Activity and Segmentation along Chenghai-Binchuan Fault Zone in Northwest Yunnan, China. Earth Science, 43(12): 4651-4670. doi: 10.3799/dqkx.2017.548

Citation:

Huang Xiaojin, Wu Zhonghai, Huang Xiaolong, Luo Ruijie, 2018. Tectonic Geomorphology Constrains on Quaternary Activity and Segmentation along Chenghai-Binchuan Fault Zone in Northwest Yunnan, China. Earth Science, 43(12): 4651-4670. doi: 10.3799/dqkx.2017.548

Citation:

Huang Xiaojin, Wu Zhonghai, Huang Xiaolong, Luo Ruijie, 2018. Tectonic Geomorphology Constrains on Quaternary Activity and Segmentation along Chenghai-Binchuan Fault Zone in Northwest Yunnan, China. Earth Science, 43(12): 4651-4670. doi: 10.3799/dqkx.2017.548

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Tectonic Geomorphology Constrains on Quaternary Activity and Segmentation along Chenghai-Binchuan Fault Zone in Northwest Yunnan, China

doi: 10.3799/dqkx.2017.548

Huang Xiaojin^{1,2,3
,},
Wu Zhonghai^{2,3
,
,},
Huang Xiaolong^2,4,
Luo Ruijie^2,5

1.
School of Civil Engineering and Architecture, Wuyi University, Wuyishan 354300, China
2.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
3.
Key Laboratory of Neotectonic Movement & Geohazard, Ministry of Land and Resources, Beijing 100081, China
4.
School of Earth and Space Sciences, Peking University, Beijing 100871, China
5.
Yunnan Earthquake Agency, Kunming 650224, China

Received Date: 2017-12-31
Publish Date: 2018-12-15

Abstract

Abstract

Chenghai-Binchuan fault zone in the southeastern margin of the Qinghai-Tibet plateau, which has a composite activity manner of vertical and horizontal left-sliding movement. It plays an important role in regulating the internal matter in the Qinghai-Tibet plateau, and controlling the major strong earthquake activity in the region. Extracting the region tectonic landforms information from the RS (remote sensing) images and DEM (digital elevation model) to quantitative study of tectonic geomorphology of the fault zone. The results show that the fault belt have the characteristics of segmented partitions. The northern boundary faults of the Jinguan-Chenghai basin are dominated by normal faults, and they have the highest vertical movement rate in the zone. Qina faults are dominated by strike-slip movement, which have the highest strike-slip activity rate. The eastern boundary faults in Binchuan basin are also dominated by normal faults. The vertical activity rate is lower than that of the northern section. Comprehensive analysis shows that the Quaternary vertical activity of Chenghai-Binchuan fault zone is lower from north to south, and strike-slip activity in central is strongest, diminishing to south. The long-term activity rate of Binchuan fault zone has maintained a relatively stable state, the vertical activity rates between 0.09-0.69 mm/a. Horizontal strike-slip rate between 0.20-1.40 mm/a. The Quaternary activity of faults mainly is "medium" and "weak", but the future earthquake risk should not be ignored, especially in the south middle of it.
- Chenghai-Binchuan fault zone,
- active fault,
- tectonic geomorphology,
- Quaternary,
- seismic hazard,
- geophysics

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References(76)

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Tectonic Geomorphology Constrains on Quaternary Activity and Segmentation along Chenghai-Binchuan Fault Zone in Northwest Yunnan, China

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