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Chromite from
Sotkavaara, Rovaniemi, Lapland, Finland


Classification
Species:Chromite
Formula:Fe2+Cr23+O4
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Chromite data
Locality Data:Click here to view Sotkavaara, Rovaniemi, Lapland, Finland
Data Identifiers
Mindat Occurrence Record ID:1266242
Long-form Identifier:1:3:1266242:3
GUID (UUID V4):30df3071-4fc5-4d07-a519-146f861e10ee
Nearest other occurrences of Chromite
28.7km (17.8 miles) ⓘSiika-KĂ€mĂ€ PGE Reef, Portimo complex, Lapland, Finland
71.6km (44.5 miles) ⓘKirakkajuppura PGE deposit, SompujĂ€rvi Reef, Penikat complex, Lapland, Finland
81.3km (50.5 miles) ⓘKompsa, Kuivaniemi, Ii, North Ostrobothnia, Finland
83.1km (51.7 miles) ⓘKylmĂ€kangas, Kuivaniemi, Ii, North Ostrobothnia, Finland
83.7km (52.0 miles) ⓘKarahkalehto (Karahka), Kuivaniemi, Ii, North Ostrobothnia, Finland
References
Reference Search (possible matching items)
Journal (article/letter/editorial)
Offset-type PGE mineralisation in the Sotkavaara Intrusion, northern Finland: an association with zones of low-cr...bGeological Survey of Finland Rovaniemi, Finland; cGeological Survey of Finland Espoo, Finland Located in northern...northern Finland, the Palaeoproterozoic Sotkavaara Intrusion was emplaced into 1.98 Ga quartz-feldspar...injections, the intrusion behaved as a closed system. Chromite crystallisation in a deeper chamber may account...values and host-rock Mg-numbers observed in the Sotkavaara Intrusion. Further, the discontinuous (rather
Journal (article/letter/editorial)
injections, the intrusion behaved as a closed system. Chromite crystallisation in a deeper chamber may account...values and host-rock Mg-numbers observed in the Sotkavaara Intrusion. Further, the discontinuous (rather
Journal (article/letter/editorial)
gneiss–migmatite crust 2550 Ma ago. It is exposed in the Kola–Lapland–Karelia Craton. The main structural features of...igneous rocks rich in Mg and Si [31], or the Kola–Lapland–Karelian plume province [32]. These Early Paleoproterozoic...Burakovsky intrusion [47], Cu-Ni-Co+PGE deposits in Finland: Kemi [39,48], Penikat [49], Portimo (Ahmavaara...were also obtained for the Ahmavaara deposits (Finland) and the Monchegorsk region (Nyud-2). Further studies...deposit (Pechenga) and the Penikat intrusion (Finland) revealed that the type of REE partition in sulfides
Journal (article/letter/editorial)
deportment: A case study of the Kevitsa mine, Finland— Louis J. Cabri, Michelle Kelvin, Zhaoping Yang...to be involved in the formation of ophiolitic chromite deposits—Zdeněk Johan, Robert F. Martin, and... J. RodrĂ­guez, L.A. Mosquea, and R. Salas 114 Chromite typology and composition characterized through...Precious metal mineralisation in the Sotkavaara Intrusion, northern Finland: Peak Pt, Pd, Au and Cu offsets
 
Mineral and/or Locality  
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