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本溪井水位地震响应范围初探
引用本文:唐光伟,贾东旭,佟薇,吴宝东.本溪井水位地震响应范围初探[J].防灾减灾学报,2014(4):27-36.
作者姓名:唐光伟  贾东旭  佟薇  吴宝东
作者单位:本溪地震台,辽宁 本溪,117022
基金项目:台站三结合基金“本溪井地下流体综合图谱集汇总及分析”
摘    要:本溪井对应地震的水位响应可分为震前响应(水位异常)和震时、震后响应(震后效应)两种。自1999年以来,本溪井多次记录到了对应典型地震较为明显的水位响应变化,最远为2004年12月26日印尼苏门答腊MS8.7地震,震中距为4990km,一般来讲,地震的震级越大,震中距越小,本溪井水位响应幅度越大。

关 键 词:本溪井  地下流体  异常  水位  地热  流量

PRELIMINARy ANALySIS OF ThE SEISMIC RESPONSE RANgE OF WATER LEVEL IN BENXI WELL
TANg guang-wei,JIA Dong-xu,TONg Wei,WU Bao-dong.PRELIMINARy ANALySIS OF ThE SEISMIC RESPONSE RANgE OF WATER LEVEL IN BENXI WELL[J].Seismological Research of Northeast China,2014(4):27-36.
Authors:TANg guang-wei  JIA Dong-xu  TONg Wei  WU Bao-dong
Institution:(Benxi Seismic Station, Liaoning Benxi 117022, China )
Abstract:The water level in Benxi Well corresponding to seismic response can be divided into pre earthquake response(the water level anomalies)and response with the earthquake, post-earthquake response (post seismic effect) . Since 1999, Benxi Well recorded many times the level corresponding to typical seismic obvious changes in response to, the farthest is December 26, 2004 Sumatra MS8.7 earthquake, epicentral distance is 4990km, generally speaking, the larger magnitude earthquake, epicentral distance is small, the water level in Benxi Well response amplitude is greater.
Keywords:Benxi Well  underground fluid  abnormalities  water level  water temperature  flow
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