摘要
用王吉易等人的地下流体附加力源的研究思路，分析了晋５—１井水位的３次高值变化，表明，这３次水位变化是华北区域应力场增强、大范围应力调整、传递的结果，反应的是华北地震活动自唐山大地震后的２个调整过程，并非简单的降雨干扰。
The 3 variations of the high value of the water level of Jin 5 1 well have been analyzed by the train of thought of the additional force source of ground fluid of Wang Jiyi,the conclusion shows that the 3 variations of the water level were the result of the strengthening of the stress field in North China,the macroscopic stress adjustment and transmission,it was the response of the 2 adjustment pocesses of the seismicity in North China after the Tangshan large earthquake,it was not a single disturbance of fall of rain.
出处
《山西地震》
1997年第4期27-31,共5页
Earthquake Research in Shanxi
