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Biotite from
Kultuma Deposit, Gazimuro-Zavodsky District, Zabaykalsky Krai, Russia


Locality type:Deposit
Classification
Species:'Biotite' (not an IMA approved species)
Formula:K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Biotite data
Locality Data:Click here to view Kultuma Deposit, Gazimuro-Zavodsky District, Zabaykalsky Krai, Russia
Data Identifiers
Mindat Occurrence Record ID:1473384
Long-form Identifier:1:3:1473384:0
GUID (UUID V4):0a76ffa9-7bc5-4d9b-90a2-17ff41f0b75e
Nearest other occurrences of Biotite
60.0km (37.3 miles) ⓘAmurskie Daiki deposit, Gazimuro-Zavodsky District, Zabaykalsky Krai, Russia
71.3km (44.3 miles) ⓘBystrinskoye Cu-Au deposit, Gazimuro-Zavodsky District, Zabaykalsky Krai, Russia
74.8km (46.5 miles) ⓘLugokanskoe deposit, Lugokan ore cluster, Gazimuro-Zavodsky District, Zabaykalsky Krai, Russia
87.3km (54.2 miles) ⓘKara ore cluster, Sretensky District, Zabaykalsky Krai, Russia
References
Kovalev, K. R., Kalinin, Y. A., Turkina, O. M., Gimon, V. O., & Abramov, B. N. (2019). Kultuminskoe gold–copper–iron–skarn deposit (Eastern Transbaikalia, Russia): Petrogeochemical features of magmatism and ore-forming processes. Russian Geology and Geophysics, 60(6), 583-601.
Redin, Yury O., Anna A. Redina, Viktor P. Mokrushnikov, Alexandra V. Malyutina, and Vladislav F. Dultsev. (2022) "Rock-Forming (Biotite and Plagioclase) and Accessory (Zircon) Minerals Geochemistry as an Indicator of the Metal Fertility of Magmas by the Example of Au-Cu-Fe-Skarn Deposits in Eastern Transbaikalia" Minerals 12, no. 1: 50. https://doi.org/10.3390/min12010050
Svetlitskaya, T. V., & Nevolko, P. A. (2022). New whole-rock skarn and porphyry fertility indicators: Insights from Cu-Au-Fe skarn and Cu-Mo-Au porphyry deposits in Eastern Transbaikalia, Russia. Ore Geology Reviews, 105108.
Redin, Yury, Redina, Anna, Malyutina, Alexandra, Dultsev, Vladislav, Kalinin, Yuri, Abramov, Bair, Borisenko, Alexander (2023) Distinctive Features of the Major and Trace Element Composition of Biotite from Igneous Rocks Associated with Various Types of Mineralization on the Example of the Shakhtama Intrusive Complex (Eastern Transbaikalia) Minerals, 13 (10) doi:10.3390/min13101334
Reference Search (possible matching items)
Redin, Yury O., Redina, Anna A., Mokrushnikov, Viktor P., Malyutina, Alexandra V., Dultsev, Vladislav F. (2021) The Kultuma Au–Cu–Fe-Skarn Deposit (Eastern Transbaikalia): Magmatism, Zircon Geochemistry, Mineralogy, Age, Formation Conditions and Isotope Geochemical Data. Minerals, 12 (1) 12 doi:10.3390/min12010012
Journal (article/letter/editorial)
minerals Article The Kultuma Au–Cu–Fe-Skarn Deposit (Eastern Transbaikalia): Magmatism, Zircon Geochemistry...Malyutina, A.V.; Dultsev, V.F. The Kultuma Au–Cu–Fe-Skarn Deposit (Eastern Transbaikalia): Magmatism...Akademika Koptyuga Avenue 3, 630090 Novosibirsk, Russia; redin@igm.nsc.ru (Y.O.R.); viktorm@igm.nsc.ru...Novosibirsk, Russia Correspondence: redina@igm.nsc.ru; Tel.: +7-913-373-0139 Abstract: The Kultuma deposit is...classification is still a controversial issue. The deposit is confined to the similarly named massif of the
Redin, Yury O., Redina, Anna A., Mokrushnikov, Viktor P., Malyutina, Alexandra V., Dultsev, Vladislav F. (2021) Rock-Forming (Biotite and Plagioclase) and Accessory (Zircon) Minerals Geochemistry as an Indicator of the Metal Fertility of Magmas by the Example of Au-Cu-Fe-Skarn Deposits in Eastern Transbaikalia. Minerals, 12 (1) 50 doi:10.3390/min12010050
Journal (article/letter/editorial)
minerals Article Rock-Forming (Biotite and Plagioclase) and Accessory (Zircon) Minerals Geochemistry...; Malyutina, A.V.; Dultsev, V.F. Rock-Forming (Biotite and Plagioclase) and Accessory (Zircon) Minerals...Akademika Koptyuga Avenue 3, 630090 Novosibirsk, Russia; redin@igm.nsc.ru (Y.O.R.); viktorm@igm.nsc.ru...of Sciences, Koptuga Ave. 3, 630090 Novosibirsk, Russia Correspondence: redina@igm.nsc.ru; Tel.: +7-913-373-0139...Transbaikalia. The largest deposits are the Lugokan, the Kultuma and the Bystrinsky. These deposits are in a paragenetic
 
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