摘要
分析了日本MS9.0地震引起的新疆温泉30井水位、水温同震变化特征。结果显示,该观测井水位同震响应和震后效应不论是响应起始时间还是阶变时间均早于水温的同震响应和震后效应的起始时间;此次日本地震引起的该观测井水温同震响应和震后效应均为阶升型,说明水位同震升降性质受控于当地的地质构造环境和水文地质条件,而水温同震变化还与地震波引起的井孔中水的运动方式、水温探头放置的位置等因素有关。
This paper analyzed characteristics of co-seismic change for water level,water temperature in No. 30 well after Japan earthquake with MS9. 0 while results showed co-seismic and aftershock effect of water level earlier than water temperature. Because of hydrogeology condition,tectonic environment,the co-seismic change of water level and water temperature were quite different from each other. The co-seismic change of water temperature was related to motion mode and location of sensor.
出处
《内陆地震》
2015年第1期37-42,共6页
Inland Earthquake
关键词
日本地震
新30井
水位水温
同震响应
震后效应
Japan earthquake
No.30 well
Water level and water temperature
Co-seismic change
Aftershock effect
