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作 者:张永双[1,2] 石菊松[1,2] 孙萍[1,2] 姚鑫[1,2]
机构地区:[1]国土资源部新构造运动与地质灾害重点实验室,北京100081 [2]中国地质科学院地质力学研究所,北京100081
出 处:《地质力学学报》2009年第2期131-141,共11页Journal of Geomechanics
基 金:中国地质调查局项目(1212010914025);地质力学所基本科研业务费项目(DZLXJK200708)资助
摘 要:内动力和外动力地质作用是地质灾害形成过程中不可缺少的两种作用,但是,以往的地质灾害研究偏重于外动力作用,对于外动力与内动力耦合作用的形式,由于缺少直观的实例,只能根据经验感觉进行判断和定性的研究。四川汶川MS8.0级地震在给人们带来灾难和损失的同时,也给人们认识内外动力耦合作用形式提供了机会。本文在龙门山地区地震地质和地质灾害调查的基础上,总结了山区地震地质灾害形成过程中内外动力耦合作用的主要表现形式,主要包括活动断裂和风化作用的耦合、岩土体结构与变形破坏形式的耦合、地震力与地形地貌的耦合以及地震力与地下水的耦合等。采用实例剖析了地震滑坡形成过程中各种地质作用及其产物之间的相互联系,对于认识地震地质灾害形成机理和发育规律具有一定的指导意义。The endogenic and exogenic geological processes are two indispensable processes for geohazard occurrence. However, the coupling between endogeni only was exogenic geological process c and exogenic geological processes widely emphasized in the past, while were only presented in formations of experiential judges and qualitative studies. The Ms8.0 Wenchuan earthquake provides a good chance to further study coupling processes between endogenic and exogenic geologic processes when it resulted in inestimable casualties and property losses. This paper summarizes the general manifestations of coupling processes in mountainous area, e structure and deformation failure, g. the couplings between active fault and weathering, rock-soil mass geomorphology and seismic force, seismic force and groundwater. An analysi has been made on the relationships seismic landslide occurrence, which will be between various geological processes and their results during of certain guiding significance for understanding seismic geohazard mechanism and its development regularity
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