Locality type: | Intrusion |
Classification |
---|
|
Species: | 'Chlorite Group' (not an IMA approved species) |
Confirmation |
---|
|
Validity: | Believed Valid |
Data |
---|
|
Mineral Data: | Click here to view Chlorite Group data |
Locality Data: | Click here to view Näränkävaara, Kuusamo, North Ostrobothnia, Finland |
Data Identifiers |
---|
|
Mindat Occurrence Record ID: | 1382955 |
Long-form Identifier: | 1:3:1382955:7 |
GUID (UUID V4): | cc712e4f-bc35-426b-81b6-82db09cee142 |
Nearest other occurrences of Chlorite Group |
---|
|
|
37.8km (23.5 miles) | ⓘKauniinvaara, Suomussalmi, Kainuu, Finland |
44.6km (27.7 miles) | ⓘAla-Luoma, Juntusranta, Suomussalmi, Kainuu, Finland |
60.6km (37.6 miles) | ⓘKonttiaho, Kuusamo, North Ostrobothnia, Finland |
60.9km (37.8 miles) | ⓘKuikkapuro deposit, Suomussalmi, Kainuu, Finland |
61.9km (38.4 miles) | ⓘSivakkaharju, Kuusamo, North Ostrobothnia, Finland |
62.0km (38.5 miles) | ⓘSäynäjävaara, Kuusamo, North Ostrobothnia, Finland |
62.1km (38.6 miles) | ⓘMeurastuksenaho, Kuusamo, North Ostrobothnia, Finland |
69.6km (43.2 miles) | ⓘKuusijärvi deposit, Koillismaa Complex, Lapland, Finland |
70.5km (43.8 miles) | ⓘJuomasuo, Kuusamo, North Ostrobothnia, Finland |
73.9km (45.9 miles) | ⓘHietaharju deposit, Suomussalmi, Kainuu, Finland |
References |
---|
|
Järvinen, V., Halkoaho, T., Konnunaho, J., Heinonen, J. S., & Rämö, O. T. (2019). Parental magma, magmatic stratigraphy, and reef-type PGE enrichment of the 2.44-Ga mafic-ultramafic Näränkävaara layered intrusion, Northern Finland. Mineralium Deposita, 1-26. |
Reference Search (possible matching items) |
---|
| Barkov, Andrei Y., Nikiforov, Andrey A., Barkova, Larisa P., Korolyuk, Vladimir N., Martin, Robert F. (2021) Zones of PGE–Chromite Mineralization in Relation to Crystallization of the Pados-Tundra Ultramafic Complex, Serpentinite Belt, Kola Peninsula, Russia. Minerals, 11 (1) 68 doi:10.3390/min11010068 | Journal (article/letter/editorial) | also to the west, to form the Tulppio belt in Finland [23]. These suites are members of a transregional...32 rocks of gabbroic affinity, i.e., gabbro or chlorite–mica–amphibole rock mapped by previous investigators...contact rocks of gabbroic affinity, i.e., gabbro or chlorite–mica–amphibole rock mapped by previous investigators...altered and replaced by a mixture of serpentine-group minerals, clinochlore, by high-resolution inductively...altered and replaced by a mixture of serpentine-group minerals, clinochlore, and Mg-rich carbonates. Fresh | | | Book | in Hainite-(Y) and Batievaite-(Y), Two Rinkite-Group Minerals from the Sakharjok Massif, Keivy Alkaline...rare earths, copper, phosphorus, niobium, platinum-group elements, and other critical metals. The continued...rare earths, copper, phosphorus, niobium, platinum-group elements, and other critical metals. The continuing...[5]. The region is also famous for its platinum-group-element (PGE) deposits, which are investigated by...ores from the Udokan (Russia) and Talvivaara (Finland) deposits, as well as technogenic waste dumps such | | | Book (volume) | similarities to any of the other three, are arranged from north to south. For Sweden, a general summary of the metallogeny...Swedish metallic ore deposits, Smalands Taberg. In Finland, a brief description of the ore geology is given...stalleites), PyhHsalmi, and Vihanti] is a separate group. These deposits show enough differences in geologic...Scotland 3 7 1 Wales Norway Sweden 1 7 17 Finland Poland USSR 12 2 30. These 80 do not include...to 15 January meeting in London of the Contact Group "Geology of Ore Deposits held at the Institute of |
|