矿震及其深井水位的异常响应  

MINING EARTHQUAKES AND ANOMALOUS RESPONSE OF GROUNDWATER LEVEL IN DEEP WELL

作　　者：车用太[1] 鱼金子[1] 马志峰 黄积刚 王尤培[3] 王琦[3] 

机构地区：[1]国家地震局地质研究所,中国北京100029 [2]枣庄市地震办公室,中国枣庄277152 [3]山东省地震局,中国济南250021

出　　处：《地震》1997年第1期61-66,共6页Earthquake

基　　金：地震科学联合基金!93015

摘　　要：简要介绍了山东省陶庄煤矿的二次矿震及其并水位的同震效应与震前异常。结果表明，矿震活动与天然地震活动在时间上有同步性，并且二次矿震的井水位同震效应形态与震前异常持续时间有差异，而这种差异主要同震源体的破坏特征有关。In this paper, two mining earthquakes and anomalous response of water level in adeep well before the earthquakes and during the earthquake's occurrence in a coalmine, Shandong province are presented. Based on the research results, the authors ad-vanced that there is a temporal synchronism between the mining and naturalearthquakes, and there are some differences between the precursory lasting time beforethe earthquakes and the curve form of water level during the earthquakeoccurrence. These differences are related to the fracture characteristics of the focal re-gion.

关 键 词：矿震 地下水位 震源动力特征 地震工程 

分 类 号：P315.9[天文地球—地震学]