Classification |
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Species: | Löllingite |
Formula: | FeAs2 |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Löllingite data |
Locality Data: | Click here to view Novye Peski deposit, Pryazhinsky District, Republic of Karelia, Russia |
Data Identifiers |
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Mindat Occurrence Record ID: | 1284960 |
Long-form Identifier: | 1:3:1284960:6 |
GUID (UUID V4): | 7f6cebcc-faf6-4a5b-bc1a-c291395277fb |
Nearest other occurrences of Löllingite |
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73.8km (45.9 miles) | ⓘPitkyaranta mining district (Pitkäranta mining district), Republic of Karelia, Russia |
73.8km (45.9 miles) | ⓘLupikko Mine, Pitkyaranta, Pitkyarantsky District, Republic of Karelia, Russia |
79.7km (49.5 miles) | ⓘKitelskoe Sn-Zn deposit (Kitelsk; Kitelskoye), Kitelya, Pitkyarantsky District, Republic of Karelia, Russia |
References |
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Ivashchenko, V. I., Bushmin, S. A., Ruchyev, A. M., Kornakov, A. S., Bogomolov, E. S., Savva, E. V., ... & Frolov, P. V. (2018, June). First Evidence of the Archean Age of Orogenic Gold of the Russian Part of the Karelian Craton (Fennoscandian Shield): Sm–Nd Mineral Isochron for Gold-Bearing Metasomatites of the Novye Peski Deposit. In Doklady Earth Sciences (Vol. 480, No. 2, pp. 804-809). Pleiades Publishing. |
Reference Search (possible matching items) |
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| Ivashchenko, V. I., Bushmin, S. A., Ruchyev, A. M., Kornakov, A. S., Bogomolov, E. S., Savva, E. V., Ivanov, M. V., Tytyk, V. M., Frolov, P. V. (2018) First Evidence of the Archean Age of Orogenic Gold of the Russian Part of the Karelian Craton (Fennoscandian Shield): Sm–Nd Mineral Isochron for Gold-Bearing Metasomatites of the Novye Peski Deposit. Doklady Earth Sciences, 480 (2) 804-809 doi:10.1134/s1028334x18060259 | Journal (article/letter/editorial) | GEOCHEMISTRY First Evidence of the Archean Age of Orogenic Gold of the Russian Part of the Karelian Craton (Fennoscandian...Isochron for Gold-Bearing Metasomatites of the Novye Peski Deposit V. I. Ivashchenkoa,*, S. A. Bushminb...Abstract—One unsolved problem of Archean metallogeny of the Russian part of the Fennoscandian Shield is...is related to the period of formation of orogenic gold deposits, the age of which was previously considered...identified the complex evolution of ores from the Novye Peski deposit and the first Neoarchean Sm–Nd isochron |
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