Opening and closing process of the Paleo-Tethys in Northern Thailand
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引用本文:Hidetoshi HARA,Koji WAKITA,Jun-ichiro KURODA,Toshiyuki KURIHARA,Katsumi UENO,Yoshihito KAMATA,Ken-ichiro HISADA,Punya CHARUSIRI,Thasinee CHAROENTITIRAT,Pol CHAODUMRONG.2009.Opening and closing process of the Paleo-Tethys in Northern Thailand[J].地球学报,30(S1):12.
DOI:10.3975/cagsb.2009.s1.08
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作者单位E-mail
Hidetoshi HARA Geological Survey of Japan, AIST, 1-1-1 Higashi, Tsukuba, Ibaraki 305-8567, Japan hara-hide@aist.go.jp 
Koji WAKITA Geological Survey of Japan, AIST, 1-1-1 Higashi, Tsukuba, Ibaraki 305-8567, Japan  
Jun-ichiro KURODA Japan Agency for Marine-Earth Science and Technology, Kanagawa 237-0061, Japan  
Toshiyuki KURIHARA Graduate School of Science and Technology, Niigata University, Niigata 950-2181, Japan  
Katsumi UENO Department of Earth System Science, Fukuoka University, Fukuoka 814-0180, Japan  
Yoshihito KAMATA Department of Earth Sciences, Yamaguchi University, Yamaguchi 753-8512, Japan  
Ken-ichiro HISADA Institute of Geoscience, University of Tsukuba, Ibaraki 305-8572, Japan  
Punya CHARUSIRI Department of Geology, Chulalongkorn University, Bangkok 10330, Thailand  
Thasinee CHAROENTITIRAT Department of Geology, Chulalongkorn University, Bangkok 10330, Thailand  
Pol CHAODUMRONG Department of Mineral Resources, Bangkok 10400, Thailand  
中文摘要:The Paleo-Tethys formed a large ocean basin that existed between Laurasia and Gondwana during Late Paleozoic to Early Mesozoic times. It opened in the Early Devonian by the rifting of Gondwanaland and closed at around latest Triassic time by the collision of the Cimmerian continent to Laurasia (Metcalfe, 1999). We reconstructed opening and closing process of the Paleo-Tethys in Northern Thailand.
中文关键词:Paleo-Tethys  total organic carbon  radiolarians  subduction  accretionary complex
 
Opening and closing process of the Paleo-Tethys in Northern Thailand
Abstract:The Paleo-Tethys formed a large ocean basin that existed between Laurasia and Gondwana during Late Paleozoic to Early Mesozoic times. It opened in the Early Devonian by the rifting of Gondwanaland and closed at around latest Triassic time by the collision of the Cimmerian continent to Laurasia (Metcalfe, 1999). We reconstructed opening and closing process of the Paleo-Tethys in Northern Thailand.
keywords:Paleo-Tethys  total organic carbon  radiolarians  subduction  accretionary complex
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