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Mayang Mine, Mayang Co., Huaihua Prefecture, Hunan Province, China
麻阳铜矿, 麻阳苗族自治县, 怀化市, 湖南省, 中国Sandstone-type copper deposit, with disseminated native copper as the main ore mineral.
Mineral List
| Azurite Calcite Chalcocite | Copper Cuprite 'Feldspar Group' | Gypsum Malachite Montmorillonite | Muscovite var: Sericite Quartz |
11 entries listed. 9 valid minerals.
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References
Manxiang Huang (1991): Petrographic analysis of the ore-bearing rock formation and prospecting guides of the Mayang copper deposit, Hunan. Geology and Prospecting 27(12), 8-12.
Qiaosong Zeng, Shinian Liu, and Manxiang Huang (2001): A study on metallogenic mechanism for Mayang copper deposit, Hunan Province. Geotectonia et Metallogenia 23(1), 42-49 (in Chinese with English abstract).
Dapeng Wang, Qian Zhang, Xiaoqing Zhu, and Zhenwei Zhang (2007): Types, characteristics and ore-forming mechanisms of native copper deposits in China. Acta Mineralogica Sinica 27(1), 57-63 (in Chinese with English abstract).
Dapeng Wang, Qian Zhang, Chaohui Zhu, Shouping Jiang, and Longbing Chen (2007): Native copper ore - Textural characteristics of the Mayang deposit and their constraints on genesis. Acta Mineralogica Sinica 27(3), 384-387 (in Chinese with English abstract).
Qiaosong Zeng, Shinian Liu, and Manxiang Huang (2001): A study on metallogenic mechanism for Mayang copper deposit, Hunan Province. Geotectonia et Metallogenia 23(1), 42-49 (in Chinese with English abstract).
Dapeng Wang, Qian Zhang, Xiaoqing Zhu, and Zhenwei Zhang (2007): Types, characteristics and ore-forming mechanisms of native copper deposits in China. Acta Mineralogica Sinica 27(1), 57-63 (in Chinese with English abstract).
Dapeng Wang, Qian Zhang, Chaohui Zhu, Shouping Jiang, and Longbing Chen (2007): Native copper ore - Textural characteristics of the Mayang deposit and their constraints on genesis. Acta Mineralogica Sinica 27(3), 384-387 (in Chinese with English abstract).
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New Locality Added: Mount Poro, Vibo Valentia Province, Calabria, ItalyFrom Ferdinando Giovine, 26th May 2013 08:11:11















