Geochronology and Petrogenesis of Late Carboniferous to Early Permian Basalts in the Central Lhasa Subterrane,Southern Tibet:Implications for the Evolution of the Sumdo Paleo-Tethys OceanOACSTPCD
Geochronology and Petrogenesis of Late Carboniferous to Early Permian Basalts in the Central Lhasa Subterrane,Southern Tibet:Implications for the Evolution of the Sumdo Paleo-Tethys Ocean
MA Wang;LIU Yingchao;YANG Zhusen;Jan-Marten HUIZENGA;LI Zhenqing;YUE Longlong;ZHAO Sibo
School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China||Institute of Geology,Sinoprobe Laboratory,Chinese Academy of Geological Sciences,Beijing 100037,ChinaInstitute of Geology,Sinoprobe Laboratory,Chinese Academy of Geological Sciences,Beijing 100037,ChinaMLR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,ChinaFaculty of Environmental Sciences and Natural Resource Management,Norwegian University of Life Sciences,NO-1432 Ås,Norway||Economic Geology Research Centre(EGRU),College of Science and Engineering,James Cook University,Townsville,Queensland 4811,Australia||Department of Geology,University of Johannesburg,Auckland Park 2006,South AfricaMLR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,ChinaInstitute of Geology,Sinoprobe Laboratory,Chinese Academy of Geological Sciences,Beijing 100037,ChinaInstitute of Geology,Sinoprobe Laboratory,Chinese Academy of Geological Sciences,Beijing 100037,China
geochemistrynorthward subductionSumdo Paleo-Tethys OceanLhasa terraneTibet
geochemistrynorthward subductionSumdo Paleo-Tethys OceanLhasa terraneTibet
《地质学报（英文版）》 2024 (4)
955-968,14
We are grateful to the staff of the Tianguansanqin Company and Xu Yutao,Mao Jingtao,and Li Jun for their assistance during the fieldwork.This research was co-supported by the National Key Research and Development Program of China(Grant No.2022YFF0800903),the National Natural Science Foundation of China(Grant Nos.42302107,92162322,42261144669,41922022,42003036),the China Geological Survey(Grant Nos.DD20243512,DD20230008),the National Postdoctoral Research Program of China(Grant No.GZC20232489),the Second Tibetan Plateau Scientific Expedition and Research(Grant No.2021QZKK0304),XingDian Youth Talent Plan of Yunnan Province(Grant No.XDYC-QNRC-2022-0136),and the UNESCO:IUGS IGCP-662 Programthis is a contribution to the latter project:'Orogen architecture and crustal growth from accretion to collision'.Constructive comments and suggestions from two anonymous reviewers significantly improved the paper.
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