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作 者:高小其[1] 王道[1] 许秋龙[1] 吴淑英[1] 卢静芳[1] 魏若萍[1] 崔勇[1]
机构地区:[1]新疆维吾尔自治区地震局,乌鲁木齐830011
出 处:《内陆地震》1999年第3期243-252,共10页Inland Earthquake
基 金:新疆地震科学基金
摘 要:依据来自哈萨克斯坦、吉尔吉斯斯坦两国地下流体的交换资料,分析了它们对天山及其邻区强震的映震特征,认为:(1)水化学异常时间与水动态异常时间不同;(2) 气体、离子、水动态异常形态多样; (3) 水化学正负异常不确定; (4) 异常幅度变化复杂; (5) 强震远场效应明显; (6) 震后效应显著并具有不可逆性。Based on the underground fluid date exchanged from Kazakhstan and Kirghizstan,the ability that they reflect strong earthquakes occurred in Tianshan and neighbouring area is analyzed. It is thought that the exchange data has following reflecting earthquake features :(1) the time of hydrochemical anomaly is different from that of water regime anomaly;(2) gas,ion and water regime have various forms of anomalies;(3) that hydrochemical anomaly is positive or negative is not definite;(4) anomalous amplitude varies complicatedly;(5) the far field effect of strong earthquakes is obvious;(6) postseismic effect is notable and irreversible.
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