Epithermal (mesothermal ?) deposit, hosted in Early Proterozoic orthogneisses and paragneisses that are overlain by Late Jurassic to Cretaceous intermediate to felsic volcanic rocks.
Ref.:
- Wu, C.Y., Bai, G., and Xu, L.M. (1993): Types and distribution of silver ore deposits in China. Mineralium Deposita 28(4), 223-239.
- Pirajno, F., Bagas, L., Hickman, A.H., and Zhejiang Gold Research Team (1997): Gold mineralization of the Chencai-Suichang Uplift and tectonic evolution of Zhejiang Province, southeast China. Ore Geology Reviews 12, 35-55.
- Mei Jianming (2000): Chemical typomorphic characteristic of pyrites from Zhilingtou gold deposit, Suichang, Zhejiang. Geoscience Journal of Graduate School of China University of Geosciences 14(1), 51-55.
- Pirajno, F., and Bagas, L. (2002): Gold and silver metallogeny of the South China Fold Belt: a consequence of multiple mineralizing events ? Ore Geology Reviews 20, 109-126.
- Khin Zaw, Peters, S.G., Cromie, P., Burrett, C., and Zengqian Hou (2007): Nature, diversity of deposit types and metallogenic relations of South China. Ore Geology Reviews 31, 3-47.
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Map Reference: 28°37'N , 119°25'E
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