摘要
结合观测环境条件,温度、大气降水等影响因素及强震响应,研究了大灰厂井氦气释放成因。结果显示,氦气释放与特殊的地质环境、温度有关,与大气降水无明显关系。
In this paper, combining with the observations of environmental condition, temperature, precipition and the response to strong earthquake,we have studied the genesis of the Helium release in the Dahuichang well. The result shows that the Helium release is relative to the special geological environment and teperature, hut to precipitation.
出处
《大地测量与地球动力学》
CSCD
北大核心
2012年第B08期81-83,97,共4页
Journal of Geodesy and Geodynamics
基金
北京市任务性科技专项(JZX-201203)
关键词
大灰厂井
八宝山断层
氦气
温度
大气降水
Dahuichang well
Babaoshan fault
Helium
temperature
precipitation
