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Geochronology and Geochemistry of the Mamupu Cu-Au Polymetallic Deposit, Eastern Tibet: Implications for Eocene Cu Metallogenesis in the Yulong Porphyry Copper Belt
投稿时间:2021-05-18  修订日期:2021-09-04  点此下载全文
引用本文:ZHANG Xiaoxu,LIN Bin,TANG Juxing,HE Liang,LIU Zhibo,WANG Qin,SHAO Rui,DU Qiu,SILANG Wangdui,CIREN Ouzhu,GUSANG Quzhen,CIDAN Zhongga.2022.Geochronology and Geochemistry of the Mamupu Cu-Au Polymetallic Deposit, Eastern Tibet: Implications for Eocene Cu Metallogenesis in the Yulong Porphyry Copper Belt[J].ACTA GEOLOGICA SINICA(English edition),96(4):1221~1236
摘要点击次数: 105
全文下载次数: 93
DOI:10.1111/1755-6724.14807
作者单位E-mail
ZHANG Xiaoxu 1 School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China 2 MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China  
LIN Bin 2 MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China linbincags@126.com 
TANG Juxing 2 MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China  
HE Liang 3 No.6 Geological Party, Tibet Bureau of Geology and Mineral Exploration and Development, Lhasa 851400, China  
LIU Zhibo 2 MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China  
WANG Qin 4 College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China  
SHAO Rui 3 No.6 Geological Party, Tibet Bureau of Geology and Mineral Exploration and Development, Lhasa 851400, China  
DU Qiu 3 No.6 Geological Party, Tibet Bureau of Geology and Mineral Exploration and Development, Lhasa 851400, China  
SILANG Wangdui 5 Tibet Shengyuan Mining Group Co., Ltd., Lhasa 851400, China  
CIREN Ouzhu 5 Tibet Shengyuan Mining Group Co., Ltd., Lhasa 851400, China  
GUSANG Quzhen 5 Tibet Shengyuan Mining Group Co., Ltd., Lhasa 851400, China  
CIDAN Zhongga 5 Tibet Shengyuan Mining Group Co., Ltd., Lhasa 851400, China  
 
Author NameAffiliationE-mail
ZHANG Xiaoxu 1 School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China 2 MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China  
LIN Bin 2 MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China linbincags@126.com 
TANG Juxing 2 MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China  
HE Liang 3 No.6 Geological Party, Tibet Bureau of Geology and Mineral Exploration and Development, Lhasa 851400, China  
LIU Zhibo 2 MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China  
WANG Qin 4 College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China  
SHAO Rui 3 No.6 Geological Party, Tibet Bureau of Geology and Mineral Exploration and Development, Lhasa 851400, China  
DU Qiu 3 No.6 Geological Party, Tibet Bureau of Geology and Mineral Exploration and Development, Lhasa 851400, China  
SILANG Wangdui 5 Tibet Shengyuan Mining Group Co., Ltd., Lhasa 851400, China  
CIREN Ouzhu 5 Tibet Shengyuan Mining Group Co., Ltd., Lhasa 851400, China  
GUSANG Quzhen 5 Tibet Shengyuan Mining Group Co., Ltd., Lhasa 851400, China  
CIDAN Zhongga 5 Tibet Shengyuan Mining Group Co., Ltd., Lhasa 851400, China  
Abstract:The Mamupu skarn-type Cu-Au polymetallic deposit represents the first discovery of a medium deposit in the southern Yulong porphyry copper belt (YPCB), eastern Tibet. The Cu-Au mineralization mainly occurs as chalcopyrite in breccia, within the plate-like carbonate interlayer, being closely related to chloritization (e.g., chlorite, magnetite and epidote) and skarnization (e.g., diopside, tremolite and garnet). The ore-related quartz syenite porphyry (QSP) and granodiorite porphyry (GP) were emplaced at 40.1 ± 0.2 Ma and 39.9 ± 0.3 Ma, respectively. The QSP of Mamupu is an alkaline-rich intrusion, relatively enriched in LREE, LILE, depleted in HFSE, with no significant negative Eu and Ce anomalies, slightly high (87Sr/86Sr)i, low εNd(t), uniform (206Pb/204Pb)i and εHf(t) values, which indicates that the porphyry magma may be caused by both the mixing of metasomatized EM II enriched mantle and thickened juvenile lower crust. The QSP in the Mamupu deposit shares a similar genesis of petrology to other ore-related porphyries within the YPCB. High oxygen fugacity and water content of the magmas are essential for the formation of porphyry and skarn Cu deposits. The QSP has similar high magmatic oxidation states and water content to the Yulong deposit, which indicates that the Mamupu has a high prospecting potential. Differences in the geological characteristics and scale of mineralization between the Mamupu and other YPCB deposits may be due to the different emplacement depths of ore-related intrusions, as well as differences in the surrounding rocks.
keywords:skarn Cu deposit, geochronology, geochemistry, Mamupu, Yulong porphyry copper belt, Tibet
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