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Deposit Area 1804 - 017
(Last updated 19.des.2017)

Name of Deposit Area : Misværdal
(Object Id : 1804,017,00,00)

Location
County : Nordland (18) Municipality : Bodø (1804)
Map 1:50000: Misvær (2029-2) Map 1:250000: Sulitjelma
Marking point: Longitude: 15.0077610 Latitude: 67.1012480
EU89-UTM Zone 33 (Coordinates IS confirmed)
X-coord: 500336 m. Y-coord: 7442667 m.

Commodity
Main Type: Special metals (Nb,Ta,Be,Li,Sc,REE) Sub Type: REE-metals
Element(s): P REE
Production
Activity: Exploration Reserves: 30000 thousand tons
Prod. method: Production:
Prod. status: Not yet active Volume of dump:
Resource estimat. standard: Non compliant

Importance
Public: Little Importance (reg. 07.12.2017)
Economical: Not classified/evaluated

Mineralization
Era: Paleozoic Period: Silurian
Dating: 440 million year Method:
Genesis: Orthomagmatic formation 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:

Information(s) in free text format
Free text
The Misværdal occurrence is a late-Ordovician to Silurian multiphase pyroxenite intrusive complex. In mineralised pyroxenite portions, apatite and allanite constitute the major and minor REE minerals, respectively. The apatite of the occurrence has attracted interest as a basic product suitable for the production of fertilizer.

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.


The fact sheet was created on 17.05.2024

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