Advances in composition and dating methods of fault gouge and weakening mechanisms of earthquake faults in bedrock area

Fault gouges result from the sliding of brittle faults and can be used to determine the deformational characteristics, formation ages and weakening mechanisms of earthquake faults, which are of great significance for structural geology and earthquake geology. Therefore, the comprehensive understandi...

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Main Authors: Xianbing Xu, Fei Deng, Dun Wang, Xiyi Luo
Format: Article
Language:zho
Published: Editorial Department of Bulletin of Geological Science and Technology 2022-09-01
Series:地质科技通报
Subjects:
Online Access:https://dzkjqb.cug.edu.cn/en/article/doi/10.19509/j.cnki.dzkq.2022.0138
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author Xianbing Xu
Fei Deng
Dun Wang
Xiyi Luo
author_facet Xianbing Xu
Fei Deng
Dun Wang
Xiyi Luo
author_sort Xianbing Xu
collection DOAJ
description Fault gouges result from the sliding of brittle faults and can be used to determine the deformational characteristics, formation ages and weakening mechanisms of earthquake faults, which are of great significance for structural geology and earthquake geology. Therefore, the comprehensive understanding of the research findings and its advances in fault gouges will contribute to palaeoseismic investigations. On the basis of collected and absorbed data, we introduced comprehensive advances in the components of fault gouges, surface textures of quartz grains from fault gouges, dating methods of fault gouges and weakening mechanisms of earthquake faults. The fault gouge is mainly composed of clay minerals and powder and debris of wall rocks. The clay minerals mainly consist of montmorillonite, illite, kaolinite and chlorite. The powder and debris of wall rocks are mainly composed of quartz, feldspar, mica, calcite and dolomite. Quartz, illite and calcite selected from fault gouges could be used to distinguish the polysstages of faulting and date its formation ages. Geochronological methods include surface texture analysis of quartz grains, electron spin resonance (ESR) and optically stimulated luminescence (OSL)dating of quartz, K-Ar or 40Ar/39Ar dating of illite, and U-Pb dating of calcite. The weakening mechanisms of earthquake faults consist of the powder of minerals, the formation of new minerals and fabric development in fault gouges, and frictional heating, frictional melting and thermal pressurization after fault initialization.
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spelling doaj.art-53b5d336f4194d4bb9c54b3c963c40de2024-03-05T02:58:18ZzhoEditorial Department of Bulletin of Geological Science and Technology地质科技通报2096-85232022-09-0141512213110.19509/j.cnki.dzkq.2022.0138dzkjtb-41-5-122Advances in composition and dating methods of fault gouge and weakening mechanisms of earthquake faults in bedrock areaXianbing Xu0Fei Deng1Dun Wang2Xiyi Luo3School of Earth Sciences, China University of Geosciences(Wuhan), Wuhan 430074, ChinaCollege of Civil Engineering, Tongji University, Shanghai 200092, ChinaSchool of Earth Sciences, China University of Geosciences(Wuhan), Wuhan 430074, ChinaFoshan Geological Bureau of Guangdong Province, Foshan Guangdong 528000, ChinaFault gouges result from the sliding of brittle faults and can be used to determine the deformational characteristics, formation ages and weakening mechanisms of earthquake faults, which are of great significance for structural geology and earthquake geology. Therefore, the comprehensive understanding of the research findings and its advances in fault gouges will contribute to palaeoseismic investigations. On the basis of collected and absorbed data, we introduced comprehensive advances in the components of fault gouges, surface textures of quartz grains from fault gouges, dating methods of fault gouges and weakening mechanisms of earthquake faults. The fault gouge is mainly composed of clay minerals and powder and debris of wall rocks. The clay minerals mainly consist of montmorillonite, illite, kaolinite and chlorite. The powder and debris of wall rocks are mainly composed of quartz, feldspar, mica, calcite and dolomite. Quartz, illite and calcite selected from fault gouges could be used to distinguish the polysstages of faulting and date its formation ages. Geochronological methods include surface texture analysis of quartz grains, electron spin resonance (ESR) and optically stimulated luminescence (OSL)dating of quartz, K-Ar or 40Ar/39Ar dating of illite, and U-Pb dating of calcite. The weakening mechanisms of earthquake faults consist of the powder of minerals, the formation of new minerals and fabric development in fault gouges, and frictional heating, frictional melting and thermal pressurization after fault initialization.https://dzkjqb.cug.edu.cn/en/article/doi/10.19509/j.cnki.dzkq.2022.0138earthquake faultfault gougecompositiondating methodweakening mechanism of fault
spellingShingle Xianbing Xu
Fei Deng
Dun Wang
Xiyi Luo
Advances in composition and dating methods of fault gouge and weakening mechanisms of earthquake faults in bedrock area
地质科技通报
earthquake fault
fault gouge
composition
dating method
weakening mechanism of fault
title Advances in composition and dating methods of fault gouge and weakening mechanisms of earthquake faults in bedrock area
title_full Advances in composition and dating methods of fault gouge and weakening mechanisms of earthquake faults in bedrock area
title_fullStr Advances in composition and dating methods of fault gouge and weakening mechanisms of earthquake faults in bedrock area
title_full_unstemmed Advances in composition and dating methods of fault gouge and weakening mechanisms of earthquake faults in bedrock area
title_short Advances in composition and dating methods of fault gouge and weakening mechanisms of earthquake faults in bedrock area
title_sort advances in composition and dating methods of fault gouge and weakening mechanisms of earthquake faults in bedrock area
topic earthquake fault
fault gouge
composition
dating method
weakening mechanism of fault
url https://dzkjqb.cug.edu.cn/en/article/doi/10.19509/j.cnki.dzkq.2022.0138
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AT dunwang advancesincompositionanddatingmethodsoffaultgougeandweakeningmechanismsofearthquakefaultsinbedrockarea
AT xiyiluo advancesincompositionanddatingmethodsoffaultgougeandweakeningmechanismsofearthquakefaultsinbedrockarea