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从天津地区近十年的地下水位变化初探本区断裂活动的新动向
PRELIMINARY STUDY ON THE TREND OF FRACTURE ACTIVETIES ACCORDING TO THE GROUNDWATER LEVEL CHANGES IN RECENT TEN YEARS IN TIANJIN AREN
【摘要】 在现有地震流体研究成果基础上,借地下水位的时空异常图象进行推测区域构造断裂活动的探索。通过对天津地区1985至1994年地下水位异常的分析对本区构造活动给出了以下推测:①1989年大同6.1级地震对地区构造活动显示出突出的调整性的变化。②沧东断裂带是本地区最活跃居主导活动地位的断裂。③沧东断裂带应力集中部位有由天津西南段向东北转移的迹象。
【Abstract】 Based on the achievements in seismological fluid research,we analysed the time and space patterns of groundwater level anomalies in the period of 1985-1994 in Tianjin area,the main results are as follows:(1) The 1989 Datong earthquake with Ms6.1 shows a adjusting change of regional tectonic activitIes ;(2) The Cangdong fractured zone is still a main active fractured zone in Tianjin area ;(3) It is found that the stress concentration position in Cangdong fractured Zone showed a kind of transfered trace from the southwestern section to the northeastern section.
- 【文献出处】 华北地震科学 ,NORTH CHINA EARTHGUAKE SCIENCES , 编辑部邮箱 ,1996年03期
- 【分类号】P315.7
- 【下载频次】63