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京、津、唐地区活动断裂带的形变特征

THE RECENT CHARACTERISTICS OF ACTIVE MAIN FAULTS IN THE BEIJING-TIANJIN-TANGSHAN REGION

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【作者】 向家翠张存德万素凡张崇立李铁明全新华

【Author】 Xiang Jia-cui, Zhang Cun-de, Wan Su-fan,Zhang Chong-li, Li Tie-ming and Quan Xin-hua(Institute of Geology, State Seismological Bureau)

【机构】 国家地震局地质研究所国家地震局地质研究所

【摘要】 本文主要利用复测水准、基线资料研究本区活动断裂的现代活动性。计算出近20条断裂的垂直运动量及少数断裂的水平运动量。根据断裂活动垂直运动年速率的水平将该区断裂分为两类,第一类1—10毫米,第二类小于1毫米。结合地震、地质资料讨论了本区活动断裂的现代活动特征。

【Abstract】 In this paper, we have studied the recent activity of main faults in these regions using geodetic data obtained from short leveling, regional leveling and short baseline measutements across faults, vertical movement values for about twenty faults have been calcalated and horizontal movement values for some faults have been also obtained from repeated leveling and baseline measurements. According to the level of fault activity, the faults may be divided into two classes, the annual vertical movement rate is 1 to 10mm for the first class, 1-0.1mm year for the second one.The recent active characteristics of these faults are discussed in combination with geological and geophysical data. There appear to be two aspects, some intensively active faults in Quaternary period have remained to be intensively active in recent years; the rate of fault activity is of no linear relation to time in these regions, suggesting an ac-celarated motion along 9 faults in an area with radius of 200km from the epicenter before Tangshan earthquake.

  • 【文献出处】 地震地质 ,Seismology and Geology , 编辑部邮箱 ,1987年03期
  • 【被引频次】4
  • 【下载频次】49
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