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地震 ›› 1998, Vol. 18 ›› Issue (1): 63-68.

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八宝山断裂带形变分析与探讨

薄万举, 谢觉民, 郭良迁   

  1. 中国天津 300180 国家地震局第一地形变监测中心
  • 收稿日期:1997-03-24 修回日期:1997-04-23 出版日期:1998-01-31 发布日期:2022-05-10
  • 作者简介:薄万举,男,1957年8月出生,高级工程师,主要从事地壳形变与地震预报研究工作。

ANALYSIS AND EXPLORATION OF DEFORMA TION OF BABAOSHAN FAULT BELT

Bo Wanju, Xie Juemin, Guo Liangqian   

  1. First Crustal Deformation Monitoring Center, SSB, Tianjin 300180, China
  • Received:1997-03-24 Revised:1997-04-23 Online:1998-01-31 Published:2022-05-10

摘要: 八宝山断裂带上布设有7处形变跨断层台点,多年来,这些台点形变资料所显示的断层活动性质差异很大,有的互相矛盾。近几年又出现了大的量级变化,是构造活动的加强还是局部环境因素的干扰,众说不一。已有的研究结果认为是干扰所致,通过进一步的实地考察,将多台点资料与地质调查结果进行综合分析,认为八宝山断裂带上观测到的形变变化的主要部分属断层构造活动所致,并非局部干扰所致。不同台点异常变化的不一致性是局部地质构造复杂程度的体现,总体上反映了NW向永定河断裂和NE向八宝山断裂变互分隔的控制作用,并且目前这种作用还比较强烈。这一研究结果对该区域现今地质构造活动的研究以及地震形变的前兆分析都有十分重要的参考价值。

关键词: 形变分析, 构造活动, 八宝山断裂带

Abstract: There are 7 deformation measuring stations and sites across the Babaoshan fault belt. For quite a few years, the data measured from the stations and sites have shown obvious difference in fault activities, and some of them are contradictory. The variation with big order of magnitude of data appeared again in recent years. There is not identical opinion whether it mainly means the strengthening of tectonic activity or the existence of interfer­ence from local environment. In some research papers it is considered that it is mainly caused by interference. Through further field investigation and comprehensive analysis of data from stations and sites and geological survey, we consider that it is mainly caused by tectonic activity rather than local interference, and the inconsistency of abnormal variation from different stations and sites is the reflection of complexity of local tectonic environ­ment. The abnormal variation generally reflected the mutual separation and controlling ef­fect between NW-striking Yongdinghe Fault and NE-striking Babaoshan Fault, and the ef­fect is now quite strong. This study result has very important reference value for research­es on current tectonic activities and analysis of earthquake deformation precursors.

Key words: Deformation analysis, Tectonic activity, Babaoshan fault belt