禾青井动水位对断层蠕动与慢地震过程的响应初析  

ANALYSIS OF THE RESPONDING OF DYNAMIC WATER LEVEL ON FAULT CREEP AND SLOW SEISMIC PROCESS IN HEQING WELL

作　　者：陈立军 

机构地区：[1]湖南省地震局,长沙410001

出　　处：《华南地震》1997年第2期39-44,共6页South China Journal of Seismology

摘　　要：以湖南禾青井深井水位观测的异常图象为例进行定性分析，发现动水位观测有可能直接反映出断层的蠕滑运动或断层的慢地震过程，前者可能为地下水物理参量的观测与研究提供新的思路，后者则可能对震源物理学的发展和地震预报水平的提高具有特殊的意义。After taking the qualitative analysis of anomalous images of deep well water level observated at Heqing well in Wunan province for example, it is found that the dynamic water level observation is probably direct to reflect the fault creep or slow seismic process. The observation of fault creep probably offers some new idea for the observation and research of the groundwater's physical parameters, and that of slow seismic process is significant on seismic source physics and earthquake prediction.

关 键 词：井水水位 断层蠕动 慢地震 地震预报 

分 类 号：P315.7[天文地球—地震学]