Locality type: | Massif |
Classification |
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Species: | 'Amphibole Supergroup' (not an IMA approved species) |
Formula: | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Amphibole Supergroup data |
Locality Data: | Click here to view Gremyakha-Vyrmes Massif, Murmansk Oblast, Russia |
Data Identifiers |
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Mindat Occurrence Record ID: | 1316368 |
Long-form Identifier: | 1:3:1316368:2 |
GUID (UUID V4): | 8b323c4b-138e-430a-ad10-3ba878bf6d48 |
Nearest other occurrences of Amphibole Supergroup |
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14.1km (8.8 miles) | ⓘSeblyavr Massif, Kolsky District, Murmansk Oblast, Russia |
87.8km (54.5 miles) | ⓘVuruchuaivench prospect, Monchegorsk, Murmansk Oblast, Russia |
91.9km (57.1 miles) | ⓘLoypishnyun deposit, Monche tundra intrusion, Murmansk Oblast, Russia |
94.4km (58.6 miles) | ⓘMount Generalskaya intrusion, Murmansk Oblast, Russia |
References |
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Arzamastsev, A. A., Bea, F., Arzamastseva, L. V., & Montero, P. (2006). Proterozoic Gremyakha-Vyrmes Polyphase Massif, Kola Peninsula: An example of mixing basic and alkaline mantle melts. Petrology, 14(4), 361-389. |
Reference Search (possible matching items) |
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| Savelyeva, V. B., Bazarova, E. P., Sharygin, V. V., Karmanov, N. S., Kanakin, S. V. (2017) Altered rocks of the Onguren carbonatite complex in the Western Tansbaikal Region: Geochemistry and composition of accessory minerals. Geology of Ore Deposits, 59 (4) 315-340 doi:10.1134/s1075701517040055 | Journal (article/letter/editorial) | Branch, Russian Academy of Sciences, Irkutsk, 664033 Russia b Institute of Geology and Mineralogy, Siberian...Novosibirsk, 630090 Russia cNovosibirsk State University, Novosibirsk, 630090 Russia d Geological Institute...Branch, Russian Academy of Science, Ulan-Ude, 670047 Russia *e-mail: vsavel@crust.irk.ru Received May 5, 2016...early-stage alteration of aluminosilicate rocks. Alkali amphibole rims grains in the higher altered rocks (Fig....with amphibole. The rocks in the inner zone of the alteration column are composed of amphibole (85– 90%) |
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