%0 Journal Article
%T 东构造节的伸展和折返:泰国北部裂谷的重力信号
%A John MILSOM
%J 地球学报
%D 2012
%R 10.3975/cagsb.2012.s1.22
%X Althoughmanyofitsdetailshavebeencriticised,theindentermodelofIndia-Asiacollision(Fig1)isstillwidelyacceptedasprovidingaworkablefirst-orderexplanationforthestructuraldevelopmentoftheeasternsyntaxisandtheinitiationofthemajorNW-SEfaultsthatsegmentthemainlandofSoutheastAsia.ArgumentshavelargelyconcernedtheextenttowhichthearrivalofthecontinentalcrustofgreaterIndiahasbeenaccommodatedbythickeningbeneaththeTibetanPlateauorbyextrusionofblocksintoSoutheastAsia.Second-orderstructuresrelevanttosuchquestionsincludeelevatedplateaus,metamorphiccorecomplexesandthenetworksofriftbasinswithbroadlyN-Strends.InnorthernThailand,onesuchriftnetworkhasbeenresponsibleforthedevelopmentofacharacteristicbasin-and-rangemorphology.
%K Gravity
%K indentermodel
%K NorthernThailand
%U http://www.cagsbulletin.com/dqxbcn/ch/reader/view_abstract.aspx?file_no=2012s122&flag=1