中国新疆温泉、哈萨克斯坦地下流体观测资料前兆异常对比与分析  

COMPARISON AND ANALYSIS OF UNDERGROUND FLUID OBSERVATION DATA PRECURSORY ANOMALY IN WENQUAN OF XINJIANG IN CHINA,KAZAKHSTAN

作　　者：汪成国[1] 朱成英[2] 杨晓芳[2] 赵刚[1] 高守权[1] 邹广[1] 陈大柱[1] 张新成[1] 

机构地区：[1]新疆维吾尔自治区地震局温泉地震台,新疆温泉县833500 [2]新疆维吾尔自治区地震局,新疆乌鲁木齐830011

出　　处：《内陆地震》2013年第3期229-234,共6页Inland Earthquake

基　　金：新疆地震科学基金(201118);中国地震局"地震监测;预测;科研"三结合课题(201261)资助

摘　　要：系统清理分析了中国新疆温泉台、哈萨克斯坦20多年地下流体观测资料。统计结果显示,中国新疆温泉台30井(泉)的氡、流量、水温,哈萨克斯坦卡帕尔井的氦气、扎尔甘特井的流量、博古特井水位、下卡姆井的氦气、萨雷扎斯井水位,映震率较高,在震前都有一定的震兆异常显示,而且前兆异常特征以高值异常为主,异常时间分布特征显示为短期异常。The authors analyzed the underground fluid observation data for twenty years in Wenquan of Xinjiang in China, Kazakhstan systematically. The statistical result showed that the Radon, flow, water temperature in No. 30 well （spring） in Wenquan of Xinjiang in China and Helium in Capar well and Shakamuka well, flow in Zardari gantt well, water level in Bogut well, and Scale well in Kazakhstan have high earthquake reflecting rate and have some earthquake precursory anomaly before the earthquakes. The precursory anomaly was high value mainly and precursory anomaly time feature was short period.

关 键 词：中国新疆温泉台 哈萨克斯坦 地下流体 前兆异常 

分 类 号：P315.72[天文地球—地震学]