2011年3月24日缅甸孟帕亚M7.2级地震地震构造浅析
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摘要
本文简要论述了2011年3月24日缅甸孟帕亚M7.2级地震的发震构造,孟帕亚断裂的活动特征、活动时代,以及断裂与历史地震活动的关系。
In this paper,we discuss briefly the seismogenic structures of Mong Hpayak M7.2 earthquake occurred on 24th March in Myanmar,the characteristics and age of Mong Hpayak fault's activity,and the relationship between the fault and the historical earthquakes are studied also.
引文
[1]Y D Sulidi-Kondrat’yev.Main features of the structure and geodynamics of laos.Geotectonics.1989,23(6):543-549
    [2]C K Morlry.Variation in late Cenozoic-recent strike-slip and oblique-exetensional geometries,within In-dochina:the influence of pre-existing fabrics,journal of structural geology,2007,29:36-58
    [3]C K Morlry.A tectonic model for the tertiary evolution of strike-slip faults and rift basins in SE Asia,tec-tonophysics.2002,347(4):189-215
    [4]P F L Smith and R B Stokes.Geology and petroleum potential of the khorat plateau basin in the Vientianearea of Laos P.D.R.journal of petroleum geology.1997,20:27-50
    [5]Anne Socquet.Cenozoic deformation in western Yunnan(China--Myanmar border).Journal of Asian EarthSciences.2005,24:495-515
    [6]常祖峰,张艳凤,陈宇军.老挝琅南塔断裂新构造活动特征与2007年班南坎MS6.6地震.地震研究,2008,31(2):124-128

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