%0 Journal Article
%T 泰国北部Inthanon带外来硅质岩块的中、晚二叠世放射虫：对与古特提斯消减有关的混杂岩形成时代的约束
%A Yoshihito KAMATA
%A Hidetoshi HARA
%A Katsumi UENO
%A Apsorn SARDSUD
%A Thasinee CHAROENTITIRAT
%A Punya CHARUSIRI
%A Ken-ichiro HISADA
%J 地球学报
%D 2012
%R 10.3975/cagsb.2012.s1.18
%X TheInthanonZoneofNorthernThailand,origi-nallyproposedbyBarrandMacdonald(1991),ischaracterizedbytheoccurrenceofPaleo-Tethyanpe-lagicsedimentsincludingCarboniferous–Permianseamount-typecarbonateassociatedwithoceanicba-salticrocksandMiddleDevonian–MiddleTriassicradiolarianchert(Ueno,1999;UenoandHisada,2001;UenoandCharoentitirat,2011).Thesepelagicrockshavebeenmainlystudiedfromtheviewpointofbio-stratigraphytoclarifythedurationoftheirdeposition.ThesestudiesconcludedthePaleo-TethystobeavastoceanbasinonceexistedbetweentheIndochinaandSibumasucontinentalblocksduringDevo-nian–Triassictimes.
%K NorthernThailand
%K Mélange
%K Radiolarian
%K Permo-Carboniferous
%U http://www.cagsbulletin.com/dqxbcn/ch/reader/view_abstract.aspx?file_no=2012s118&flag=1