| Citation: | Siyuan Wang, Qibing Xiao, Jianguo Zeng. Tectonic Dynamic Metallization of Silver-Gold Hydrothermal Fluids in Proterozoic Gneiss Terrene Shear Zones, Suichang, Zhejiang, China. Journal of Earth Science, 2001, 12(1): 68-74.
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The Suichang mine is the largest silified vein-type silver-gold mineralization system in Southeast China, whose ore bodies are controlled by shear zones developing in Lower Proterozoic gneiss terrene with initial migmatization, which is covered by Upper Jurassic and Lower Cretaceous volcanic rock system and cut by acidic igneous veins of Jurassic and Cretaceous. The conclusions are as follows: (1) The ore-forming fluid is defined as superhigh tectonic-metamorphic fluid on the base of: ①
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