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Columbia超大陆汇聚在扬子陆块西南缘的响应——来自热液石英脉锆石U-Pb年龄的证据
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引用本文:LIU Junping,WANG Xiaohu,GUAN Xueqing,DENG Renhong,YIN Wei,LUO Guangming,TIAN Sumei. Response of Columbia supercontinent convergence to the southwestern margin of Yangtze Block: Evidence from zircon U-Pb age of hydrothermal quartz vein[J]. Geology in China, 2021, 48(5): 1653-1654(in Chinese with English abstract).
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Author NameAffiliationE-mail
LIU Junping Yunnan Institute of Geological Survey, Kunming 650216, Yunnan, China
School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China
Key Laboratory of Sanjiang Metallogeny and Resources Exploration and Utilization, MNR, Kunming, 650051, Yunnan, China 
 
WANG Xiaohu Yunnan Institute of Geological Survey, Kunming 650216, Yunnan, China
Key Laboratory of Sanjiang Metallogeny and Resources Exploration and Utilization, MNR, Kunming, 650051, Yunnan, China 
339078312@qq.com 
GUAN Xueqing Yunnan Institute of Geological Survey, Kunming 650216, Yunnan, China  
DENG Renhong Yunnan Institute of Geological Survey, Kunming 650216, Yunnan, China  
YIN Wei Yunnan Institute of Geological Survey, Kunming 650216, Yunnan, China  
LUO Guangming Yunnan Institute of Geological Survey, Kunming 650216, Yunnan, China  
TIAN Sumei Yunnan Institute of Geological Survey, Kunming 650216, Yunnan, China
Key Laboratory of Sanjiang Metallogeny and Resources Exploration and Utilization, MNR, Kunming, 650051, Yunnan, China 
 
基金项目:本文为云南省1∶5万撒马基幅、因民幅、贵城幅、舒姑幅区域地质调查(D201905)资助的成果。
 
Response of Columbia supercontinent convergence to the southwestern margin of Yangtze Block: Evidence from zircon U-Pb age of hydrothermal quartz vein
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