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Study on Holocene Paleoearthquakes in Xizhang Trench on the Jiaocheng Fault Zone,Shanxi Province

Xie Xinsheng Sun Changbin Yan Chengguo Zhao Jinquan Jiang Wali An Weiping Li Zihong Zhang Dawei Cheng Xinyuan Gao Shuyi Wang Chunhe

中国地震研究(英文版)2008,Vol.22Issue(4):428-439,12.
中国地震研究(英文版)2008,Vol.22Issue(4):428-439,12.

Study on Holocene Paleoearthquakes in Xizhang Trench on the Jiaocheng Fault Zone,Shanxi Province

Study on Holocene Paleoearthquakes in Xizhang Trench on the Jiaocheng Fault Zone,Shanxi Province

Xie Xinsheng 1Sun Changbin 2Yan Chengguo 1Zhao Jinquan 2Jiang Wali 2An Weiping 2Li Zihong 2Zhang Dawei 2Cheng Xinyuan 3Gao Shuyi 1Wang Chunhe1

作者信息

  • 1. Institute of Crustal Dynamics,China Earthquake Administration,Beijing 100085,China
  • 2. Earthquake Administration of Shanxi Province,Taiyuan 030000,China
  • 3. Jinei Seismological Station,Earthquake Administration of Shanxi Province,Taiyuan 030000,China
  • 折叠

摘要

Abstract

Xizhang trench is located 10 km northwest of Taiyuan city,Shanxi Province,in front of a NNW-trending scarp of 4.6m height on the northern segment of the Jiaocheng fault zone.The dimensions of the trench are 108m in length,8m in width,and 10m in depth.There are 18 horizons revealed in the trench.The upper strata are sandy loam;the upper strata of the downthrown block of the fault are gravels,the lower ones are an interbed of brown loam and sandy loam.The strata on the upthrown block of the fault are sandy loam containing gravel.The trench shows 3 fault planes,and the upper offset point on the fault plane is 1.5m below the ground surface,the newest dislocated stratum is (3.74±0.06)ka BP.The trench reveals a lot of deformation traces,such as fault planes,dislocated strata,collnvial wedges and formation tilting.The relationship between strata and faults in the trench shows that 3 paleoearthquake events have occurred at the Jiaocheng fault zone since the Early Holocene,they are about (3.74+0.06)~(3.06±0.26)ka BP,(8.35±0.09)ka~ (3.74±0.06)ka BP,and(10.66±0.85)~(8.35±0.09)ka BP.The average interval among the events is 2.6~3.6ka.The minimum coseismic vertical displacements of the 3 events are 3.0m,2.5m and 3.2m,respectively.The significance of Xizhang trench is that the Jiaocbeng fault used to be active thousands of years ago,though there is no M≥ 7.0 earthquake recorded in historical documents.Evidence of new Jiaocheng fault zone activity during the Holocene is important for the earthquake safety assessment of Taiyuan city in the future.

关键词

Paleoearthquake/Holocene/Xizhang trench/Jiaocheng fault/Shanxi

Key words

Paleoearthquake/Holocene/Xizhang trench/Jiaocheng fault/Shanxi

分类

天文与地球科学

引用本文复制引用

Xie Xinsheng,Sun Changbin,Yan Chengguo,Zhao Jinquan,Jiang Wali,An Weiping,Li Zihong,Zhang Dawei,Cheng Xinyuan,Gao Shuyi,Wang Chunhe..Study on Holocene Paleoearthquakes in Xizhang Trench on the Jiaocheng Fault Zone,Shanxi Province[J].中国地震研究(英文版),2008,22(4):428-439,12.

基金项目

This project was sponsored by the program of"Active Fault Test Detection in City" of the National Development and Reform Commission,PRC. ()

中国地震研究(英文版)

2096-9996

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