《Table 3 S-Pb isotope composition of sulfide and sulphosalts from the Baiyangping Pb-Zn polymetallic

《Table 3 S-Pb isotope composition of sulfide and sulphosalts from the Baiyangping Pb-Zn polymetallic   提示:宽带有限、当前游客访问压缩模式
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《"Metallogeny of the Baiyangping Lead-Zinc Polymetallic Ore Concentration Area, Northern Lanping Basin of Yunnan Province, China"》


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The east ore belt consists of the Hexi,Dongzhiyan,Xiaquwu,Yanzidong,Huachangshan,Huishan,and Heishan ore deposits/blocks,which are located along the NNE-striking Huachangshan thrust fault(Figs.2 and 5;Table 1).The west ore belt consists of the Baiyangping,Liziping,Wudichang and Fulongchang ore blocks(Fig.6).The ore bodies are hosted in Mesozoic sandstones and carbonates,and occur in three faults of nearly North-South(N-S-striking),West-Northwest(WNW),and NortheastSouthwest(NE-SW),respectively(Fig.6;Table 1).