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): |
South Muya Range |
Political location(s): |
Russia |
Deposit clan (type): |
sediment-hosted copper |
Deposit (sub) types: |
undifferentiated; in sandstone and siltstone horizon |
Geologic province: |
Siberian Platform |
Commodities: |
Cu |
Geological ages: |
Early Proterozoic (host rocks) |
Host rocks: |
(1) sedimentary; sandstone-siltstoneIndividual lithologies: | sandstone siltstone | Host rock stratigraphy: | Samodurovka Suite |
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Qualified comments: |
(Applies to: miscellaneous comments) in sandstone and siltstone horizon; visible part of cupriferous horizon is 9 km long in metamorphosed rock; mode of origin of Vitim & Udokan cupriferous rocks are similar |
References: |
Narkelyun, L. F.; Bezrodnykh, Y. P.; Kulakov, M. A., 1969 |
Copper Potential of Sedimentary Bodies in South of Siberian Platform |
International Geology Review, Volume 11, p. 288 - 297 |
Salikhov, V. S., 1975 |
Postsedimentation Changes in Copper-Bearing Deposits of the South Siberian Platform |
International Geology Review, Volume 17, p. 83 - 94 |
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