发震断裂带内黏土矿物的纳微米变形

晁洪太; 王志才; 王雷; 孙岩

doi:10.3799/dqkx.2018.426

Volume 43 Issue 5

May 2018

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Article Navigation > Earth Science > 2018 > 43(5): 1746-1754

Chao Hongtai, Wang Zhicai, Wang Lei, Sun Yan, 2018. Nano/Micro-Scale Deformation of Clay Minerals in Seismogenic Fault Zone. Earth Science, 43(5): 1746-1754. doi: 10.3799/dqkx.2018.426

Citation:

Chao Hongtai, Wang Zhicai, Wang Lei, Sun Yan, 2018. Nano/Micro-Scale Deformation of Clay Minerals in Seismogenic Fault Zone. Earth Science, 43(5): 1746-1754. doi: 10.3799/dqkx.2018.426

Chao Hongtai, Wang Zhicai, Wang Lei, Sun Yan, 2018. Nano/Micro-Scale Deformation of Clay Minerals in Seismogenic Fault Zone. Earth Science, 43(5): 1746-1754. doi: 10.3799/dqkx.2018.426

Citation:

Chao Hongtai, Wang Zhicai, Wang Lei, Sun Yan, 2018. Nano/Micro-Scale Deformation of Clay Minerals in Seismogenic Fault Zone. Earth Science, 43(5): 1746-1754. doi: 10.3799/dqkx.2018.426

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Nano/Micro-Scale Deformation of Clay Minerals in Seismogenic Fault Zone

doi: 10.3799/dqkx.2018.426

1.
Earthquake Administration of Shandong Province, Jinan 250014, China
2.
School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, China

Received Date: 2017-10-01
Publish Date: 2018-05-15

Abstract

Abstract

Fault gouge is one of the most obvious material indicators in seismogenic fault zone, and it retains a wealth of information of fault activities. Based on field investigation and observation under microscope, nano/micro-scale deformation styles of clay minerals in seismogenic fault zone were analyzed in detail and discussed in this paper by use of SEM technology. The clay minerals are arranged in alignment during stick-slipping, and exhibit parallel extinction zones under orthogonal polarization microscope. In the view of SEM, the directional arrangement of flake clay minerals can be observed, and multiple stick-slipping events on the principle sliding zone can be clearly identified. Moreover, it is found that the creep-slipping phenomena in fault gouges are universal. In the microscopic view, clay minerals exhibit wavelike extinction zones. In the view of SEM, fold deformation, wavelike deformation, sliding around the gravels and entangling deformation of flake clay minerals can be observed. As stick-slipping and creep-slipping indications can be observed in the same view, and by analyzing their temporal relationship, it is found that the creep-slipping occurs before the stick-slipping and corresponds to the movement in the meta-instability stage of fault sliding.
- nano/micro-scale deformation,
- clay mineral,
- seismogenic fault,
- stick-slipping,
- creep-slipping,
- earthquake,
- tectonics

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References(77)

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Nano/Micro-Scale Deformation of Clay Minerals in Seismogenic Fault Zone

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