Locality type: | Reef |
Classification |
---|
|
Species: | Violarite |
Formula: | Fe2+Ni23+S4 |
Confirmation |
---|
|
Validity: | Believed Valid |
Data |
---|
|
Mineral Data: | Click here to view Violarite data |
Locality Data: | Click here to view Rometölväs reef, Pudasjärvi, North Ostrobothnia, Finland |
Data Identifiers |
---|
|
Mindat Occurrence Record ID: | 854385 |
Long-form Identifier: | 1:3:854385:1 |
GUID (UUID V4): | 27850fb7-0acd-4b12-a29b-d7cedd8328b3 |
Nearest other occurrences of Violarite |
---|
|
|
32.7km (20.3 miles) | ⓘKuusijärvi deposit, Koillismaa Complex, Lapland, Finland |
84.3km (52.4 miles) | ⓘSiika-Kämä PGE Reef, Portimo complex, Lapland, Finland |
84.7km (52.6 miles) | ⓘHietaharju deposit, Suomussalmi, Kainuu, Finland |
95.0km (59.0 miles) | ⓘKilvenjärvi Offset Sulfide-PGE Deposit, Portimo complex, Lapland, Finland |
References |
---|
|
|
Reference Search (possible matching items) |
---|
| | Journal (volume) | GEOLOGICAL SURVEY OF FINLAND • Bulletin 404 • Tuomo Karinen www.gtk.fi info@gtk.fi This study deciphers...sulphidemineralized layer referred to as the Rometölväs Reef of the 2440 Ma old Koillismaa Intrusion. The...that the origin of the mineralization of the Rometölväs Reef was triggered by emplacement of dykes of a...the noncumulus-textured gabbronorite bodies of the reef. ISBN 978-952-217-092-7 (paperback) ISBN 978-952-217-093-4...GEOLOGICAL SURVEY OF FINLAND Bulletin 404 2010 The Koillismaa Intrusion, northeastern Finland – evidence for | | | Book | Mineral Deposits of Finland Edited by Wolfgang D. Maier Raimo Lahtinen Hugh O’Brien AMSTERDAM • BOSTON...Geological Survey of Finland, Espoo, Finland I. Haapala University of Helsinki, Helsinki, Finland T. Halkoaho...Geological Survey of Finland, Kuopio, Finland E. Hanski Oulu Mining School, Oulu, Finland A. Hartikainen Geological...Geological Survey of Finland, Kuopio, Finland C. Hartshorne AngloAmerican Exploration, London, UK T....Mawson Resources, Finland E. Heilimo Geological Survey of Finland, Kuopio, Finland P. Heino Yara Suomi |
|