Database name: |
World Sediment-Hosted Cu Deposits |
Compilers: |
R. V. Kirkham, J. J. Carriere, A. Rafer, and P. Born |
Release date: |
2015-01-27 |
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Deposit name(s): |
Kandrykul |
Political location(s): |
Russia; Province or state: Ural Mountains |
Deposit clan (type): |
sediment-hosted copper |
Deposit (sub) types: |
paralic marine; in marine beds of gray sandstone above red beds |
Geologic province: |
Russian Platform |
Commodities: |
Cu |
Geological ages: |
Kazanian (host rocks) |
Host rocks: |
(1) sedimentary; carbonate-sandstoneIndividual lithologies: | sandstone (grey) limestone |
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Qualified comments: |
(Applies to: miscellaneous comments) in marine beds of gray sandstone above red beds; Mansfeld type/ Cu confined to basal sandstone & limestone; lingula unit overlies Kazanian sequence which overlies Ufimian stage |
References: |
Davidson, C. F., 1965 |
A Possible Mode of Origin of Strata-Bound Copper Ores |
Economic Geology, Volume 60, p. 942 - 954 |
Lurye, A. M., 1972 |
Mineralization of the Mansfeld Type in the Upper Permian of the West Ural Region |
Doklady Akademii Nauk SSSR, Volume 203, p. 61 - 63 |
Lur'ye, A. M.; Gablina, I. F., 1972 |
The Copper Source in Production of Mansfeld-Type Deposits in the West Ural for eland |
Geochemistry International, Volume 9, p. 56 - 67 |
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