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English version | ||||
| MALMDATABASEN | |||||
| Forekomstområde 1804 - 017 | |||||
| (Sist oppdatert 19.des.2017) | |||||
Navn på deposit area : Misværdal |
| (Objekt Id : 1804,017,00,00) |
| Lokalisering |
| Fylke : | Nordland (18) | Kommune : | Bodø (1804) |
| Kart 1:50000: | Misvær (2029-2) | Kart 1:250000: | Sulitjelma |
| Markeringspunkt: | Lengdegrad: | 15.0077610 | Breddegrad: | 67.1012480 |
| EU89-UTM Zone 33 | (Coordinates IS confirmed) |
| X-koord: | 500336 m. | Y-koord: | 7442667 m. |
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| Materialtype |
| Hovedtype: | Spesialmetaller (Nb,Ta,Be,Li,Sc,REE) | Subtype: | REE-metaller | |
| Element(s): | P REE |
| Production |
| Activity: | Prospektering | Reserves: | 30000 thousand tons | |
| Prod. method: | Production: | |||
| Prod. status: | Ikke satt i drift | Volume of dump: | ||
| Resource estimat. standard: | Ikke standardisert |
| Betydning |
| Offentlig: | Little Importance (reg. 07.12.2017) |
| Economical: | Ikke vurdert |
Mineralization |
| Era: | Paleozoic | Period: | Silurian | |
| Dating: | 440 million year | Method: | ||
| Genesis: | Ortomagmatisk | Form: | ||
| Main texture: | Min. distribution: |
| Main grain size: | Main alteration: |
| Strike/Dip: | Direction: | |||
| Plunge: |
| Stratigraphic classification of host rock |
| Era: | Paleozoic | Period: |
| Province: | ||
| Geotec.unit: | ||
| Tectonic complex: | ||
| Igneous complex: |
| Group: | Formation: |
Bibliography: |
| From NGU's Reference Archive: |
| Ihlen, Peter M.; Schiellerup, Henrik; Gautneb, Håvard; Skår, Øyvind , 2014 |
| Characterization of apatite resources in Norway and their REE potential — A review |
| ;Elsevier;ARTIKKEL;Ore geology reviews; No.58;126-147 pages |
| Abstract: | |
| Apatite is a necessity for the production of phosphorus fertilizers and presents a potential raw material for the extraction of REE and Y. A wide spectrum of apatite deposits is found in Norway including sedimentary, igneous, and vein type deposits. The igneous deposits which appear to have the greatest potential for exploitation occur associated with alkaline complexes, massif-type anorthosite complexes and monzonitic complexes. One of the most promising is found in the monzonoritic Bjerkreim–Sokndal Layered Intrusion of the early Neoproterozoic Rogaland Anorthosite Province in southwest Norway. |
| Faktaarket ble generert 13.06.2026 |
| Spørsmål eller kommentarer vedrørende faktaarket kan mailes til: ressursdatabaser@ngu.no |
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