| 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 | |
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| 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 |
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| Opening and closing process of the Paleo-Tethys in Northern Thailand |
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| 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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