Abstract
The Tangganshan manganese ore deposit is a typical sedimentary-magmatic hydatopneumatogenic superimposed ore deposit. In this paper this deposit is discussed in more detail from the following aspects: geology, ore mineralogy, and geochemistry. On the basis of its occurrence, mineral assemblage, element geochemistry, isotopic geochemistry, and characteristics of organic matter and fluid inclusions, the Tangganshan manganese ore deposit has proved to be a new-type manganese ore deposit that has been enriched by magmatic-pneumatolic solutions. Most of the ore-forming elements were derived from the ore deposit itself, and the rest from the magmatic-pneumatolitic solutions.
Similar content being viewed by others
References
Fan Liangming et al.,Bulletin of Chengdu Geological College, 2(1983), 30–34(in Chinese).
Zhang Baogui et al.,Geochimica, 4(1982), 393–402(in Chinese).
Tu Guangchi et al., “Geochemistry of China’s Stratabound Ore Deposits” Science Press, Beijing, Vol. 1(1984), 8(in Chinese).
Zhang Shoufan, “Mineralogy”, Commercial Publishing House, Beijing, 1954, 250(in Chinese).
Institute of Geochemistry, Academia Sinica, “Geochemistry of Granitoids in South China”, Science Press, Beijing, 1979, 278–303(in Chinese).
Wang Liankui et al., Memoirs of Geochemistry (No. 1), Science Press, Beijing, 1984, 1–4(in Chinese).
Zhang Jiuling,Geology and Exploration, 2(1982), 26–40(in Chinese).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Baogui, Z., Guoxi, C. & Jingyu, C. Mineralogy and geochemistry of a stratabound manganese deposit in the Tangganshan region of South China. Chin. J. of Geochem. 7, 67–75 (1988). https://doi.org/10.1007/BF02840431
Issue Date:
DOI: https://doi.org/10.1007/BF02840431