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Shenghua Wu
Chinese Academy of Sciences
3Publications
2H-index
6Citations
Publications 3
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#1Shenghua Wu (CAS: Chinese Academy of Sciences)H-Index: 2
#2Jingwen MaoH-Index: 1
Last.Weidong Sun (CAS: Chinese Academy of Sciences)H-Index: 48
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Abstract Scheelite has been analyzed from the Shizhuyuan and the Xianglushan world-class W deposits from the Nanling W–Sn region and Jiangnan W belt, respectively. The Shizhuyuan deposit consists of proximal skarn and greisen W–Sn–Mo–Bi and distal Pb–Zn–Ag veins. The Xianglushan deposit, contains layer-like sulfide–scheelite and skarn W orebodies on granite cupolas overprinted by W greisen veins. Scheelite in skarn ores from the Shizhuyuan contains higher concentrations of Mo than those in the s...
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#1Shenghua Wu (CAS: Chinese Academy of Sciences)H-Index: 2
#2Weidong Sun (CAS: Chinese Academy of Sciences)H-Index: 48
Last.Xudong Wang (NU: Northeastern University)H-Index: 2
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Abstract The Dongyuan deposit, in the recently identified world-class porphyry–skarn W metallogenic belt, east Jiangnan Orogen, China, is characterized by a set of nearly parallel and horizontal multi-cycle orebodies within cupolas of porphyritic granodiorite. Almost every orebody from the top to the bottom shows similar vertical changes in vein morphology and mineral assemblage from ≤1 cm quartz–feldspar–scheelite–calcite veins to 1–2 cm quartz–feldspar–muscovite–scheelite veins to 2–5 cm quart...
2 CitationsSource
#1Pan DaiH-Index: 2
#2Jingwen MaoH-Index: 35
Last.Xiaohong LuoH-Index: 3
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Abstract The Xianglushan W deposit in northwestern Jiangxi Province, South China, is one of numerous large-size W deposits along the northern margin of the Jiangnan Massif. The deposit comprises lenticular and stratiform-like orebodies, mainly along the contact between argillaceous limestone of the Cambrian Yangliugang Formation and a biotite granite pluton. The mineralization is zoned from proximal W greisen within the cupolas of the biotite granite, through W skarn and sulfide-scheelite bands ...
4 CitationsSource
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