|
|
English version | ||||
| MALMDATABASEN | |||||
| Forekomstområde 623 - 022 | |||||
| (Sist oppdatert 16.mar.2020) | |||||
Navn på deposit area : Skuterud Nordgruver |
| (Objekt Id : 0623,022,00,00) |
| Forekomstområdet tilhører provinsen : Modum Vest |
| Lokalisering |
| Fylke : | Buskerud (06) | Kommune : | Modum (0623) |
| Kart 1:50000: | Hokksund (1714-1) | Kart 1:250000: | Skien |
| Markeringspunkt: | Lengdegrad: | 9.8637970 | Breddegrad: | 59.9777870 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-koord: | 548211 m. | Y-koord: | 6649252 m. |
|
|
| Materialtype |
| Hovedtype: | Jernlegeringsmetaller (Cr,Ni,Co,V,Mo,W) | Subtype: | Kobolt | |
| Element(s): | Co Cu As |
| Production |
| Activity: | Gruvedrift | Reserves: | ||
| Prod. method: | Dag- og underjordsdrift | Production: | 140 thousand tons | |
| Prod. status: | Nedlagt | Volume of dump: |
| Betydning |
| Offentlig: | Not Assessed (reg. 09.02.2017) |
| Economical: | Kan være viktig , (Confirmed 06.mai.2015 by Terje Bjerkgård) |
Products |
| Element/product | Crude ore grade or quality | |
| CO | 0.2 % |
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: |
| Bilde(r) fra forekomstområdet: |
|
Bibliography: |
| From NGU's Reference Archive: |
| Grorud, Hans-Fredrik , 1997 |
| Textural and compositional characteristics of cobalt ores from the Skuterud Mines of Modum, Norway |
| ;Norsk geologisk forening;TIDSSKRIFTARTIKKEL;Norsk geologisk tidsskrift; No.77 (1);31-38 pages |
| Abstract: | |
| The metasedimentary rocks of the Modum Complex contain concordant, sulphide- rich zones, commonly referred to as 'fahlbands'. Two of these fahlbands contain cobalt minerals. Petrographic and microprobe analyses of the cobalt minerals have been performed on selected samples, to gain insight into the genesis and post-mineralization history of the cobalt minerals. It is suggested that these minerals precipitated from an oxidizing fluid, and that certain minerals in the uraninite.thorianite series precipitated simulataneously. The fahlband silicates, and later the cobalt minerals, were recrystallized during Sveco- norwegian penetrative deformation and thermal maximum (-1.2- -0.9Ga). Prolonged heating during this event eradicated any compositional zoning which may originally have been present. Neither textural nor mineral chemical analyses indicate whether the observed cobalt minerals are the result of a primary precipitation, or of remobilization. |
Navn på locality : Gruve 6 |
| (Objekt Id : 0623,022,01,00) |
| Lokalisering |
| Fylke : | Buskerud (06) | Kommune : | Modum (0623) |
| Kart 1:50000: | Hokksund (1714-1) | Kart 1:250000: | Skien |
| Markeringspunkt: | Lengdegrad: | 9.8652970 | Breddegrad: | 59.9796440 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-koord: | 548292 m. | Y-koord: | 6649459 m. |
|
|
| Materialtype |
| Hovedtype: | Jernlegeringsmetaller (Cr,Ni,Co,V,Mo,W) | Subtype: | Kobolt | |
| Element(s): | Co As |
| Faktaarket ble generert 19.06.2026 |
| Spørsmål eller kommentarer vedrørende faktaarket kan mailes til: ressursdatabaser@ngu.no |
| Copyright © 2026 Norges geologiske undersøkelse |