|
Norsk versjon | ||||
| THE ORE DATABASE | |||||
| Deposit Area 1867 - 011 | |||||
| (Last updated 13.feb.2026) | |||||
Name of Deposit Area : Selvåg prospekt |
| (Object Id : 1867,011,00,00) |
| Location |
| County : | Nordland (18) | Municipality : | Bø (1867) |
| Map 1:50000: | Nykvåg (1132-1) | Map 1:250000: | Svolvær |
| Marking point: | Longitude: | 14.5677130 | Latitude: | 68.7704850 |
| EU89-UTM Zone 33 | (Coordinates IS confirmed) |
| X-coord: | 482531 m. | Y-coord: | 7628831 m. |
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| Commodity |
| Main Type: | Ferrous metals(Fe, Mn, Ti) | Sub Type: | Iron-Titanium | |
| Element(s): |
| Importance |
| Public: | (No data) |
| Economical: | Not classified/evaluated |
Mineralization |
| Era: | Period: | |||
| Dating: | Method: | |||
| Genesis: | Form: | |||
| Main texture: | Min. distribution: |
| Main grain size: | Main alteration: |
| Strike/Dip: | Direction: | |||
| Plunge: |
| Stratigraphic classification of host rock |
| Era: | Period: |
| Province: | ||
| Geotec.unit: | ||
| Tectonic complex: | ||
| Igneous complex: |
| Group: | Formation: |
Information(s) in free text format |
| Free text |
| Arealet er basert på overflatekartlegging og oversiktskartet som er presentert hos Priesemann og Krause (1985). For informasjon ellers, se Selvåg-forekomsten, hvis utstrekning utgjøres av mere detaljerte undersøkelser og malmberegninger utført av Elkem a/S på 1980-tallet. |
Bibliography: |
| From NGU's Reference Archive: |
| Priesemann, F.D.; Krause, H. , 1985 |
| The Selvåg deposit: a proterozoic magmatic Fe-Ti-V occurrence on Vesterålen, Northern Norway. |
| ;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU Bulletin; No.402;51-64 pages |
| Abstract: | |
| The Selvåg Fe-Ti-V deposit is hosted by the Eidet-Hovden layered intrusion situated within the Precambrian Lofoten-Vesterålen province. The igneous complex is of olivine-tholeiitic affinity and shows a strong iron-enrichment trend. The deposit lies within the upper ore horizon (UZc) of the layered series. Faulting has resulted in two separate heterogenous ore bodies characterized by strong modal layering. The ore consists of titanomagnetite with ulvøspinel and ilmenite lamellae, ilmenite and sulphides. The mode of titanomagnetic relative to ilmenite show little variation in their compositions. The northern ore body contains the most valuable ore reserves with 44 Mt probable ore with about 25 wt.% V. The southern lens is of minor economic importance. |
| The fact sheet was created on 15.02.2026 |
| Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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