摘要
通过对1980—1995年青海省3．2m地温距平场与年降水量距平％场、年地震释放总能量的相关分析，指出：若某地区地温异常偏高且干旱少雨，则未来该区可能发生地震。因3．2m地温变化缓慢，该结论具有一定的预报意义。
The relation between the distance average of the 3. 2m depth geotemperature and me distance average field of yearly precipitation and yearly amount of seismic energy release is alialysed in this paper. The result shows that if it is drought with less raining and the temperature is extreamly high, the earthquake will occur in this area. Because the geotemperature of 3. 2mdepth changes slowly, the result has certain predictional significance.
出处
《高原地震》
1997年第1期69-73,共5页
Plateau Earthquake Research
关键词
地温场
降水量
地震
地温异常
Geothermal field
Precipitation
Earthquake
Geotemperature anomaly
