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(英文)  

Middle and Late Permian Radiolarians from Allochthonous Chert Blocks in the Inthanon Zone,Northern Thailand:Constraints for the Formation Age of Mélange Fabric Related to Paleo-Tethys Subduction

作　　者：Yoshihito KAMATA Hidetoshi HARA Katsumi UENO Apsorn SARDSUD Thasinee CHAROENTITIRAT Punya CHARUSIRI Ken-ichiro HISADA 

机构地区：[1]Graduate School of Life and Environmental Sciences,University of Tsukuba,Ibaraki,Japan [2]Geological Survey of Japan,AIST,1-1-1 Higashi,Tsukuba,Ibaraki 305-8567,Japan [3]Department of Earth System Science,Faculty of Science,Fukuoka University,Fukuoka 814-0180,Japan [4]Bureau of Geological Survey,DMR,Bangkok 10400,Thailand [5]Department of Geology,Faculty of Science,Chulalongkorn University,Bangkok 10330,Thailand

出　　处：《地球学报》2012年第S1期36-37,共2页Acta Geoscientica Sinica

摘　　要：The Inthanon Zone of Northern Thailand,originally proposed by Barr and Macdonald(1991),is characterized by the occurrence of Paleo-Tethyan pelagic sediments including Carboniferous-Permian seamount-type carbonate associated with oceanic

关 键 词：Northern Thailand MÉLANGE RADIOLARIAN PERMO-CARBONIFEROUS 

分 类 号：P5[天文地球—地质学]