Analysis of coseismic effect on temperature in the Three Gorges well network

Through the Three Gorges well network, we examine different coseismic changes in water temperature caused by local earthquakes since 2008, and offer a mechanistic explanation.The relations between the coseismic changes in water temperature and the parameters of distant and local earthquakes are dedu...

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Bibliographic Details
Published inGeodesy and Geodynamics Vol. 6; no. 1; pp. 61 - 66
Main Authors Zhang, Weihua, Wang, Qiuliang, Li, Jinggang, Luo, Junqiu, Guo, Xizhi
Format Journal Article
LanguageEnglish
Published Elsevier B.V 2015
KeAi Communications Co., Ltd
Subjects
Amptitude
Coseismic effect
Epicenter distance
Focal mechanism
Local earthquake
Magnitude
Three Gorges well network
Well water temperature
三峡井网
同震效应
地震参数
水温
温度
网络
Amptitude
Coseismic effect
Well water temperature
Local earthquake
Epicenter distance
Magnitude
Three Gorges well network
Focal mechanism
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Summary:Through the Three Gorges well network, we examine different coseismic changes in water temperature caused by local earthquakes since 2008, and offer a mechanistic explanation.The relations between the coseismic changes in water temperature and the parameters of distant and local earthquakes are deduced.
Bibliography:Zhang Weihua, Wang Qiuliang, Li Jinggang, Luo Junqiu, Guo Xizhi（ a Key Laboratory of Earthquake Geodesy, Institute of Seismology, China Earthquake Administration, Wuhan 430071, China b Wuhan Base of Institute of Crustal Dynamics, China Earthquake Administration, Wuhan 430071, China c Key Seismic Monitoring Station of the Three Gorges Project Ecological and Environmental Monitoring System, Wuhan 430071, China）
Three Gorges well network Coseismic effect Local earthquake Well water temperature Magnitude Epicenter distance Focal mechanism
Through the Three Gorges well network, we examine different coseismic changes in water temperature caused by local earthquakes since 2008, and offer a mechanistic explanation.The relations between the coseismic changes in water temperature and the parameters of distant and local earthquakes are deduced.
42-1806/P
ISSN:1674-9847
DOI:10.1016/j.geog.2014.12.005