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Extensional Setting of Hainan Island in Mesoproterozoic: Evidence from Granitic Intrusions in the Baoban Group
投稿时间:2021-07-02  修订日期:2021-12-22  点此下载全文
引用本文:LIU Yuheng,MAO Jingwen,QIU Kunfeng,HU Jun,WANG Lei,XU Deming.2022.Extensional Setting of Hainan Island in Mesoproterozoic: Evidence from Granitic Intrusions in the Baoban Group[J].ACTA GEOLOGICA SINICA(English edition),96(4):1199~1212
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DOI:10.1111/1755-6724.14907
作者单位E-mail
LIU Yuheng 1 MNR Key Laboratory of Geochemical Exploration, Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang, Hebei 065000, China 2 UNESCO International Centre on Global-scale Geochemistry, Langfang, Hebei 065000, China  
MAO Jingwen 3 MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China 4 China University of Geosciences (Beijing), Beijing 100083, China jingwenmao@263.net 
QIU Kunfeng 5 State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, China  
HU Jun 6 Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, Shandong 266100, China 7 Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao, Shandong 266237, China  
WANG Lei 8 Wuhan Center of China Geological Survey (Central South China Innovation Center for Geosciences), Wuhan 430205, China  
XU Deming 8 Wuhan Center of China Geological Survey (Central South China Innovation Center for Geosciences), Wuhan 430205, China  
 
Author NameAffiliationE-mail
LIU Yuheng 1 MNR Key Laboratory of Geochemical Exploration, Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang, Hebei 065000, China 2 UNESCO International Centre on Global-scale Geochemistry, Langfang, Hebei 065000, China  
MAO Jingwen 3 MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China 4 China University of Geosciences (Beijing), Beijing 100083, China jingwenmao@263.net 
QIU Kunfeng 5 State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, China  
HU Jun 6 Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, Shandong 266100, China 7 Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao, Shandong 266237, China  
WANG Lei 8 Wuhan Center of China Geological Survey (Central South China Innovation Center for Geosciences), Wuhan 430205, China  
XU Deming 8 Wuhan Center of China Geological Survey (Central South China Innovation Center for Geosciences), Wuhan 430205, China  
Abstract:The Mesoproterozoic Baoban Group is the oldest basement in Hainan Island and has played an important role in Columbia (Nuna) supercontinent reconstructions. The Mesoproterozoic granitic intrusions in the Baoban Group are the most widely-exposed Precambrian magmatic rocks and are the key to understanding the tectonic settings of Hainan Island and its relationship with the South China Block and the Columbia supercontinent. New LA-ICP-MS zircon U-Pb dating on three mylonitic granite samples from the Tuwaishan and Baoban areas yield ages ranging from 1447 Ma to 1437 Ma, representing the absolute timing of the emplacement of the granitic intrusions. Combined with previously published geochronological data for rocks from the Baoban Group and regional mafic intrusions, it is concluded that the Baoban Group formed at 1460–1430 Ma, coeval with the emplacement of the granitic and mafic intrusions. New in-situ zircon Lu-Hf isotope analyses for the three mylonitic granite samples yielded positive εHf(t) values, ranging from +0.49 to +8.27, with model ages (TCDM) ranging from 2181 Ma to 1687 Ma, suggesting that the granitic intrusions originated from a mixed source of Paleoproterozoic crust with juvenile crust. New zircon trace element data show characteristics of high Th/U values of 0.24–1.50, steep slopes from LREE to HREE and negative Pr, Eu anomalies with positive Ce, Sm anomalies, representing typical magmatic zircons formed in continental crust. Compared with available magmatic and detrital zircon ages from Precambrian rocks in the Cathaysia Block, Yangtze Block and western Laurentia, it is inferred that Hainan Island was separated from both the Cathaysia Block and the Yangtze Block, instead being connected with western Laurentia in the Columbia supercontinent. Considering the decreasing tendency of basin deposition time along the western margin of Laurentia, it is proposed that Hainan Island was located to the north or northwest of the Belt-Purcell Supergroup, along the western margin of Laurentia, during the breakup of the Columbia supercontinent.
keywords:zircon U-Pb dating, Lu-Hf isotopes, granitic intrusions, Baoban Group, extensional setting, Hainan Island
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