Sulfur Isotopes Geochemistry of the Nage Cu-Pb Polymetallic Deposit, Southeast Guizhou Province, China
来源期刊:矿物学报2009年增刊第1期
论文作者:LIU Yong-kun LONG Xuan-lin HUANG Zhi-long BAO Guang-ping YANG De-zhi FAN Liang-wu ZHOU Jia-xi WANG Jing-song
摘 要: The Nage Cu-Pb polymetallic deposit is located in the transitional zone of the Yangtze craton and cathaysia, that is the southwest of Jiangnan orogenic belt. The mainly strata are Wentong formation of Mesoproterozoic Sibo group and the Jialu formation (Qbj) , Wuye formation (Qbw) , Fanzhao formation (Qbf) and Gongdong formation (Qbg) of the Neoproterozoic Qingbaikou System Xiajiang group.
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摘要: The Nage Cu-Pb polymetallic deposit is located in the transitional zone of the Yangtze craton and cathaysia, that is the southwest of Jiangnan orogenic belt. The mainly strata are Wentong formation of Mesoproterozoic Sibo group and the Jialu formation (Qbj) , Wuye formation (Qbw) , Fanzhao formation (Qbf) and Gongdong formation (Qbg) of the Neoproterozoic Qingbaikou System Xiajiang group.
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