吕惠琴, 黄振义, 李朝弼, 李振清, 孟祥顺. 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[J]. 华北地震科学, 1996, 14(3): 38-47.
引用本文: 吕惠琴, 黄振义, 李朝弼, 李振清, 孟祥顺. 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[J]. 华北地震科学, 1996, 14(3): 38-47.
lu Huiqin, Huang Zhenyi, Li Chaobi, Li Zhenqing, Meng Xiangshun. PRELIMINARY STUDY ON THE TREND OF FRACTURE ACTIVETIES ACCORDING TO THE GROUNDWATER LEVEL CHANGES IN RECENT TEN YEARS IN TIANJIN AREN[J]. North China Earthquake Sciences, 1996, 14(3): 38-47.
Citation: lu Huiqin, Huang Zhenyi, Li Chaobi, Li Zhenqing, Meng Xiangshun. PRELIMINARY STUDY ON THE TREND OF FRACTURE ACTIVETIES ACCORDING TO THE GROUNDWATER LEVEL CHANGES IN RECENT TEN YEARS IN TIANJIN AREN[J]. North China Earthquake Sciences, 1996, 14(3): 38-47.

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.

     

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