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新疆及哈萨克斯坦地下流体氦气震兆特征

Seismic precursor features for Helium of underground fluid in Xinjiang and Kazakhstan

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【作者】 杨晓芳崔勇高小其张涛热孜万古力·艾买提

【Author】 Yang Xiaofang;Cui Yong;Gao Xiaoqi;Zhang Tao;Reziwanguli·Aimaiti;Earthquake Administration of Xinjiang Uygur Autonomous Region;

【机构】 新疆维吾尔自治区地震局

【摘要】 分析新疆10泉、04泉及哈萨克斯坦卡帕尔—阿拉善4井、下卡姆卡井氦气(He)含量变化的源兆、场兆、远兆的映震特征,地震前兆异常表现为:上升(或下降)幅度、速率变化超出正常范围,具有较好的重复性,测值遵循背景值—趋势性上升(或突升)—恢复至背景值;趋势性下降(或突降)—恢复至背景值的变化过程。各监测点氦气异常形态、异常持续时间、异常幅度同源兆、场兆、大震远兆没有明显的关系;由于各观测点的水文地质条件和地球化学环境不同,不同监测点氦气映震能力有较大差异,其中新10号泉和卡帕尔—阿拉善4井氦气的映震能力较强。

【Abstract】 In this paper,the seismic precursor features for helium of No.KKNo.4 spring in Xinjiang and No.4 well of Kaparr-Alashan,Shakamuka well in Kazakhstan are analyzed.The precursor features for helium shown as:The rising range and velocity change repeatedly exceeded normal range;background value showed an increasing or decreasing tendency and then recovered.There is not obvious relationship between anomaly curve,anomalous duration,anomalous amplitude of helium and source precursor,field precursor,far-field precursor in each observation point.Because of various hydrogeology condition and geochemical environment,earthquake reflecting ability of helium had a greater difference in some observation point,for instance:No.10 spring and No.4 well of Kaparr-Alashan are far more better than No.4spring and Shakamuka well.

【基金】 新疆地震局青年科学基金项目(201108);中国地震局震情跟踪合同制任务(2012020309)联合资助
  • 【文献出处】 地震地磁观测与研究 ,Seismological and Geomagnetic Observation and Research , 编辑部邮箱 ,2013年Z1期
  • 【分类号】P315.72
  • 【被引频次】1
  • 【下载频次】32
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