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作 者:SONG Hao SONG Shiwei
机构地区:[1]Chengdu University of Technology [2]Institute of Mineral Resources,Chinese Academy of Geological Sciences
出 处:《Acta Geologica Sinica(English Edition)》2015年第2期689-690,共2页地质学报(英文版)
基 金:financially supported by China Geological Survey (grant no.12120113095500);the National Basic Research Program of China (973 Program) (grant no.2015CB453000);the Foundation of China Nuclear Geology (grant no.201148)
摘 要:This study focused on the typical Precambrian copper- iron-gold-uranium deposits in the southwestern margin of the Yangtze block, such as the Lala in Huili, Dahongshan in Xinping, Yinachang in Wuding, and Chahe in Yuanjiang. Through systematically sampling of rocks, mineral and single mineral samples, this study discussed the continental geodynamics, age of magmatic rocks and metallogenic epoch, coupling relationship between polymetallic elements and ore-forming fluid, and the coupling relationship between magma evolution and polymetallic mineralization based on the latest metallogenic theory and modern analytical techniques.This study focused on the typical Precambrian copper- iron-gold-uranium deposits in the southwestern margin of the Yangtze block, such as the Lala in Huili, Dahongshan in Xinping, Yinachang in Wuding, and Chahe in Yuanjiang. Through systematically sampling of rocks, mineral and single mineral samples, this study discussed the continental geodynamics, age of magmatic rocks and metallogenic epoch, coupling relationship between polymetallic elements and ore-forming fluid, and the coupling relationship between magma evolution and polymetallic mineralization based on the latest metallogenic theory and modern analytical techniques.
关 键 词:Re-Os Dating of Chalcopyrite from the Lala IOCG Deposit in the Kangdian Copper Belt China OS
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