Opornyi pegmatite, Zunshibir' valley, Ermakovskoe Be Deposit, Buriatia Republic (Buryatia), Transbaikalia (Zabaykalye), Eastern-Siberian Region, Russia
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| Location is approximate, estimate based on other nearby localities. | |
|---|---|
| Latitude & Longitude (WGS84): | 51° North , 109° East (est.) |
| Margin of Error: | ~1km |
| Other regions containing this locality: | Siberian Federal District, Russia Soviet Union (1922-1991) |
| Locality type: | Pegmatite |
| Köppen climate type: | Dwc : Monsoon-influenced subarctic climate |
| Name(s) in local language(s): | Опорный , падь Зуншибирь |
Point of betafite mineralization into granitic pegmatite, opened during estabishing of high-voltage power line bearings on Southern slope Zunshibir' valley about 1 km S from Ermakovskoe Be deposit.
Mineral List
12 valid minerals.
Rock Types Recorded
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References
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Mironov A.G. and Gofman A.F, (1979) Barian betafite in pegmatites of Transbaikalien, - Minerals and Minerals Paragenesisa of Rocks and Ores, Leningrad, Nauka, p.127-132 (in Russian).
Opornyi pegmatite, Zunshibir' valley, Ermakovskoe Be Deposit, Buriatia Republic, Transbaikalia, Eastern-Siberian Region, Russia