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THE INDUSTRIAL MINERAL DATABASE
Deposit Area 1870 - 321
(Last updated 23.apr.2024)

Name of Deposit Area : Vikeid vest
(Object Id : 1870,321,00,00)

Location
County : Nordland (18) Municipality : Sortland (1870)
Map 1:50000: Myre (1232-4) Map 1:250000: Svolvær
Marking point: Longitude: 15.2434740 Latitude: 68.7613550
EU89-UTM Zone 33 (Coordinates IS confirmed)
X-coord: 509843 m. Y-coord: 7627772 m.

Commodity
Main Type: Graphite Sub Type:

Production
Activity: Exploration Reserves: 29630 thousand tons
Prod. method: Production:
Prod. status: Volume of dump:

Importance
Public: National Importance (reg. 05.10.2023)
Economical: Significant , (Confirmed 05.okt.2023 by Havard Gautneb)

Products
Element/product Crude ore grade or quality
REFRAC 11,3 %

Mineralization
Era: Period:
Dating: Method:
Genesis: Form:
Main texture: Min. distribution:
Main grain size:
Strike/Dip: Direction:
Plunge:
Stratigraphic classification of host rock
Era: Period:
Province:
Geotec.unit:
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Igneous complex:
Group: Formation:

Information(s) in free text format
Free text
The Vikeid West area is almost 100 % soil covered. Graphite schist was observed in a few drainage channels in 1991 (Gautneb & Tveten 1992). However, neither the relationships to the country rocks, nor the structure and the deformation of the rock can be observed in the field. The drilling gave a complete profile through one of the graphite sections at this locality. Rønning 2019) Analysis of 12 samples from the area show an average TC content of 10.4 % and a maximum value of 16.7 %. The graphite appears as flakes with industrial interesting size. The TC content of twelve samples varies from 0.5 % to 16.7 % with an average value of 10.4 %. One drill-hole intersects graphite mineralisation for > 20 m but is directed away from the best conducting part. The TC content in the drill-core is ca. 5 % in massive parts, and ca. 1 % in disseminated parts. However, this drill-hole is located at the rim of Structure I and probably does not describe the real total carbon content in the mineralisation. The graphite appears as good flake quality with grain size from ca. 0.1 mm to several mm. The Vikeid West area (Vikeidet) is among the most interesting graphite mineralisation in Vesterålen It is the regards as the same occurences as Vedåsen

Bibliography:
From NGU's Reference Archive:
Rønning, J.S.;Gautneb, H.; Larsen, B.E.; Baranwal, V.C.; Davidsen, B.; Engvik, A.K.; Gellein, J.; Knezevic, J.; Ofstad, F.; Xiuyan Ren; Viken, G. , 2019
Geophysical and geological investigations of graphite occurrences in Vesterålen, Northern Norway, in 2018 and 2019
;Norges geologiske undersøkelse;RAPPORT;NGU-rapport; No.2019.031;212 pages
Abstract:
Several potential graphite occurrences in Vesterålen were selected for follow-up work based on helicopter-borne geophysical data. The purpose for this is to confirm the existence of the graphite and next to briefly evaluate the quality and quantity of the graphite-bearing structures. The goal for the project, which is sponsored by Nordland county administration, is to increase the knowledge of each individual graphite occurrence. By doing so, the interest in graphite prospecting in Northern Norway may increase, effective prospecting can be implemented, and land planning can be developed with appropriate regard for areas with potential for economic graphite.

Gautneb, Håvard; Tveten, Einar , 1992
Grafittundersøkelser og geologisk kartlegging på Langøya, Sortland kommune, Nordland.
;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.92.155;78 pages
Abstract:
Rapporten omhandler NGUs grafittundersøkelser og geologiske kartlegging som har vært utført i tilknyttning til grafittforekomstene ved Jennestad. Undersøkelsene har resultert i en betydelig utvidelse av området for potensi- elle grafittforekomster. I Jennestad - Vikeid området har det blitt utført røsking og prøvetaking av grafittskifer på ca. 20 lokaliteter. De geologiske forhold og grafittens kvalitet rapporteres. Det har blitt boret 7 hull, til- sammen ca. 250 m. Det har blitt funnet flere lokaliteter med grov flakig grafitt med gehalter opptil 40 %. Grafittskiferen er assosiert med pyroksen- gneis, amfibolitt og dolomitt. Opptreden av grafittskifer synes sterkt domi- nert av strukturgeologiske forhold.


The fact sheet was created on 17.05.2024

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