泰国北部Inthanon带混杂岩碎屑锆石U-Pb年龄及碎屑岩岩石学和地球化学研究:对古特提斯消减和汇聚的启示
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引用本文:Hidetoshi HARA,Miyuki KUNII,Ken-ichiro HISADA,Katsumi UENO,Yoshihito KAMATA,Punya CHARUSIRI,Thasinee CHAROENTITIRAT.2012.泰国北部Inthanon带混杂岩碎屑锆石U-Pb年龄及碎屑岩岩石学和地球化学研究:对古特提斯消减和汇聚的启示[J].地球学报,33(s1):15.
DOI:10.3975/cagsb.2012.s1.08
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作者单位E-mail
Hidetoshi HARA Geological Survey of Japan, AIST hara-hide@aist.go.jp 
Miyuki KUNII Graduate School of Life and Environmental Sciences, University of Tsukuba  
Ken-ichiro HISADA Graduate School of Life and Environmental Sciences, University of Tsukuba  
Katsumi UENO Department of Earth System Science, Fukuoka University  
Yoshihito KAMATA Graduate School of Life and Environmental Sciences, University of Tsukuba  
Punya CHARUSIRI Earthquake and Tectonic Geology Research Unit, Chulalongkorn University  
Thasinee CHAROENTITIRAT Earthquake and Tectonic Geology Research Unit, Chulalongkorn University  
中文摘要:The accretionary complex related to the Pa-leo-Tethys subduction was developed along western margin of the Indochina Block in northern Thailand. The provenance, source rock compositions, and sedi-ment supply system of the accretionary complex were reconstructed based on the petrography and geochem-istry of clastic rocks, U-Pb dating of detrital zircons.
中文关键词:U-Pb Age  detrital zircon  Inthanon zone  Northern Thailand
 
Petrography and Geochemistry of Clastic Rocks, U-Pb Ages of Detrital Zircon from Mélange within the Inthanon Zone, Northern Thailand: Implications for Paleo-Tethys Subduction and Convergence
Abstract:The accretionary complex related to the Pa-leo-Tethys subduction was developed along western margin of the Indochina Block in northern Thailand. The provenance, source rock compositions, and sedi-ment supply system of the accretionary complex were reconstructed based on the petrography and geochem-istry of clastic rocks, U-Pb dating of detrital zircons.
keywords:U-Pb Age  detrital zircon  Inthanon zone  Northern Thailand
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