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地球学报  2012 

东构造节的伸展和折返:泰国北部裂谷的重力信号

DOI: 10.3975/cagsb.2012.s1.22

Keywords: Gravity,indentermodel,NorthernThailand

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Abstract:

Althoughmanyofitsdetailshavebeencriticised,theindentermodelofIndia-Asiacollision(Fig1)isstillwidelyacceptedasprovidingaworkablefirst-orderexplanationforthestructuraldevelopmentoftheeasternsyntaxisandtheinitiationofthemajorNW-SEfaultsthatsegmentthemainlandofSoutheastAsia.ArgumentshavelargelyconcernedtheextenttowhichthearrivalofthecontinentalcrustofgreaterIndiahasbeenaccommodatedbythickeningbeneaththeTibetanPlateauorbyextrusionofblocksintoSoutheastAsia.Second-orderstructuresrelevanttosuchquestionsincludeelevatedplateaus,metamorphiccorecomplexesandthenetworksofriftbasinswithbroadlyN-Strends.InnorthernThailand,onesuchriftnetworkhasbeenresponsibleforthedevelopmentofacharacteristicbasin-and-rangemorphology.

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