Kaneda, H., Shimazaki, H., Lee, M. S. (1986) Mineralogy and geochemistry of the Au-Ag ore deposits of the South Korean Peninsula. Mineralium Deposita, 21 (3) 234-243 doi:10.1007/bf00199806
Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | Mineralogy and geochemistry of the Au-Ag ore deposits of the South Korean Peninsula | ||
Journal | Mineralium Deposita | ||
Authors | Kaneda, H. | Author | |
Shimazaki, H. | Author | ||
Lee, M. S. | Author | ||
Year | 1986 (July) | Volume | 21 |
Page(s) | 234-243 | Issue | 3 |
Publisher | Springer Science and Business Media LLC | ||
DOI | doi:10.1007/bf00199806Search in ResearchGate | ||
Mindat Ref. ID | 155456 | Long-form Identifier | mindat:1:5:155456:8 |
GUID | 2746bc5f-2396-4147-98a4-446214cfe08b | ||
Full Reference | Kaneda, H., Shimazaki, H., Lee, M. S. (1986) Mineralogy and geochemistry of the Au-Ag ore deposits of the South Korean Peninsula. Mineralium Deposita, 21 (3) 234-243 doi:10.1007/bf00199806 | ||
Plain Text | Kaneda, H., Shimazaki, H., Lee, M. S. (1986) Mineralogy and geochemistry of the Au-Ag ore deposits of the South Korean Peninsula. Mineralium Deposita, 21 (3) 234-243 doi:10.1007/bf00199806 | ||
In | (1986, July) Mineralium Deposita Vol. 21 (3) Springer Science and Business Media LLC |
References Listed
These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.
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Papunen, H.: Sulfide mineralization of the Kotalahti and Hitra nickel-copper ores, Finland. Ann Acad. Sci. Fennicae, A III 109:1–74 (1970) | |
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Urashima, Y.: Au-Ag deposits in Japan. In: Gold-Silver ores in Japan I. Urashima, Y. (ed). J. Min. Metall. Inst. Japan. pp. 1–42 (1975) | |
Yamaoka, K., Nedachi, M.: Gold- and silver-minerals from the Chitose and the Takatama epithermal ore deposits. In: Goldsilver ores in Japan II. Urashima, Y. (ed). J. Min. Metall. Inst. Japan. pp. 75–100 (1978) |
See Also
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