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Tracing Disrupted Outer Margin of Paleoeurasian Continent through Union of Myanmar
作者姓名:Myo Min  Khin Khin Lin
作者单位:Myo Min Khin Khin LinDepartment of Geology,University of Mandalay,Mandalay,MyanmarFeng Qinglai Faculty of Earth Sciences,China University of Geosciences,Wuhan 430074Chongpan ChonglakmaniSchool of Geotechnology,Suranaree University of Technology,Na
基金项目:GermanAcademicExchangeService(DAAD)
摘    要:INTRODUCTIONDuringthepasttwodecades ,amajorityofgeoscientistshaveregardedmainlandSoutheastAsiaascomposedofGond wana derivedterraneswhichcrossed“Paleotethys”tocollidewiththeformerPaleoeurasiancontinentinLateTriassic/Juras sic (Metcalfe ,1999;ScoteseandGolonk…


Tracing Disrupted Outer Margin of Paleoeurasian Continent through Union of Myanmar
Myo Min,Khin Khin Lin.Tracing Disrupted Outer Margin of Paleoeurasian Continent through Union of Myanmar[J].Journal of China University of Geosciences,2001,12(3).
Authors:Ingavat-Helmcke Rucha  Khin Khin Lin  Helmcke Dietrich  Dieter Meischner  Feng Qinglai  Myo Min  Chongpan Chonglakmani
Abstract:Based on stratigraphy, facies distribution and paleontology of upper Paleozoic and Triassic strata in Malaysia, Thailand, Myanmar and Yunnan (China), the location of the division between the outer margin of the disrupted Paleoeurasian continent and possible Gondwana derived terranes is discussed. It is proposed that this division is located much further to the west than that has usually been maintained.
Keywords:Southwest Asia  Paleotethys  tectonic  boundary between Gondwana and Paleoeurasian continents  
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