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Adaptability of ESR dating of fault gouge in aseismic region: A case study on Hangzhou region, China

YAO Qi CHEN Han-lin ZHANG Wei YE Jian-qing LIU Jing-wei ZHAO Dong NIU Jia-wen LIAO Lin

地震学报(英文版)2008,Vol.21Issue(3):267-274,8.
地震学报(英文版)2008,Vol.21Issue(3):267-274,8.

Adaptability of ESR dating of fault gouge in aseismic region: A case study on Hangzhou region, China

Adaptability of ESR dating of fault gouge in aseismic region: A case study on Hangzhou region, China

YAO Qi 1CHEN Han-lin 2ZHANG Wei 1YE Jian-qing 2LIU Jing-wei 1ZHAO Dong 2NIU Jia-wen 3LIAO Lin4

作者信息

  • 1. Department of Earth Sciences, Zhefiang University, Hangzhou 310027, China
  • 2. Basin Structural Research Center, Chinese Education Ministry, Hangzhou 310027, China
  • 3. Engineering Seismology Institute of Zhejiang Province, Hangzhou 310013, China
  • 4. State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China
  • 折叠

摘要

Abstract

ESR dating has been widely used in seismic assessment. In this paper, we collected fault gouge samples system-atically for ESR (Electron Spin Resonance) dating, and sediment samples of overlying strata, and offset strata for OSL (Optically Stimulated Luminescence) dating along Xiaoshan-Qiuchuan fault (XQF) trending NE-SW, Xiaofeng-Sanmen fault (XSF) trending NW-SE, and Changhua-Putuo fault (CPF) trending E-W. In the same fault outcrop, the ESR data of fault gouge is greater than the OSL data of the strata offset by fault. Therefore, the ESR data of fault gouge colleted in Hangzhou region do not represent the time of weak fault movement in Late Quater-nary region, but represent the strong fault movements in Late Cenozoic. The episode of fault movement in Late Cenozoic could be speculated according to the ESR data: 1.00-0.58 Ma, there were strong fault movements along the XSE XQF and CPF in Hangzhou region; 0.58~0.45 Ma, the fault movements of all faults became weaker and did not zero ESR signals significantly for ESR dating of fault movements; 0.45~0.20 Ma, there were strong fault movements along part of XQF; 0.1~0.01 Ma, there were fault movements along the XSF only, but the fault move-ments were not strong enough to reset the ESR signal; Since 0.01 Ma, the Hangzhou region tends to be stable. In addition, the XSF might be the division line of fault segmentation of XQF; there were strong fault movements along the southwest segment of XQF during 0.45 Ma to 0.20 Ma; while the fault movements along the northeast segment of XQF mainly occurred during 1.00-0.58 Ma.

关键词

fault gouge/ ESR dating/ fault activity/ Xiaoshan-Qiuchuan fault/ Hangzhou region

Key words

fault gouge/ ESR dating/ fault activity/ Xiaoshan-Qiuchuan fault/ Hangzhou region

分类

天文与地球科学

引用本文复制引用

YAO Qi,CHEN Han-lin,ZHANG Wei,YE Jian-qing,LIU Jing-wei,ZHAO Dong,NIU Jia-wen,LIAO Lin..Adaptability of ESR dating of fault gouge in aseismic region: A case study on Hangzhou region, China[J].地震学报(英文版),2008,21(3):267-274,8.

基金项目

Project of the Tenth Five-year Plan of Hangzhou Goverment and Earthquake Administration of Hangzhou(HZZFCG-2005-A4) (HZZFCG-2005-A4)

地震学报(英文版)

1000-9116

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