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关于汶川大地震的几个地质问题

Some Geologic Questions About Wenchuan Violent Earthquake

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【作者】 孙玮罗志立杨荣军刘树根雍自权代寒松

【Author】 SUN Wei~a,LUO Zhi-li~b,YANG Rong-jun~b,LIU Shu-gen~c,YONG Zi-quan~b,DAI Han-song~b(Chengdu University of Technology,a.College of Earth Sciences;b.College of Energy Resources;c.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu,Sichuan 610059,China)

【机构】 成都理工大学地球科学学院成都理工大学能源学院成都理工大学油气藏地质及开发工程国家重点实验室

【摘要】 通过对发生汶川大地震的龙门山断裂带的地质构造背景分析,结合龙门山断裂带浅部和深部构造特征,回答了人们关注的几个构造地震问题,认为汶川大地震是陆内俯冲(C-俯冲)引起的构造地震,可能为双震余震型地震,因而震级大、破坏性强。并通过对比龙门山断裂带和成都平原的发震地质条件,认为成都平原处于稳定的扬子古板块内,不存在发生大地震的地质条件。

【Abstract】 The analysis of the geologic tectonic background and structural units division of Longmenshan fault belt where the Wenchuan violent earthquake happened in May 2008 replies the questions about tectonic earthquakes,combined with sallow and deep structural characters of Longmenshan fault belt.It is indicated that Wenchuan violent earthquake belongs to tectonic earthquake resulted from intracontinental subduction(C-subduction),probably being the type of double major shocks plus aftershocks.Hence,it has high magnitude and intensive destruction.By comparison of the geologic conditions causing the earthquake of Longmenshan fault belt with Chengdu plain,it is believed that a big earthquake could not take place in Chendu plain for it locates within the stable ancient Yangtze plate.

  • 【文献出处】 新疆石油地质 ,Xinjiang Petroleum Geology , 编辑部邮箱 ,2009年01期
  • 【分类号】P542
  • 【被引频次】7
  • 【下载频次】236
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