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Occurence 0 - 000 FEIL | |||||
(Object Id: ) (Last updated: 13.02.2024) |
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Location |
County: | Municipality: | Mangler () |
Map 1:50000: | Fjotland (1412-3) | Map 1:250000: | Mandal |
Coordinate system: | UTM-Zone 33 - EUREF89/WGS84 |
East: | 388300 m. | North: | 6506300 m. |
Longitude: | 7.0734890 | Latitude: | 58.6811270 |
Show on map |
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Resource |
Resource Type: | Ferroalloys (Cr,Ni,Co,V,Mo,W) | Resource Subtype: | Molybdenium | |
Element(s): | Mo |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Resources and production |
Activity: | Test mining | Reserves: | ||
Operating method: | Underground mining | Historical production: |
Products |
Element/product | Crude ore grade or quality | Reg. date | |
MoS2 | 0,23 % | 13.02.2024 |
Operations |
From - To | Activity | Comments | |
1916 - 1919 | Test mining | Company/Institution :A/S Ørnehommen molybdengruber |
Mineralization |
Era: | Proterozoic | Period: | Neoproterozoic | |
Genesis: | Hydrothermal vein | Form: | ||
Main texture: | Structureless | Min. distribution: | Irregular (scattered) |
Main grain size: | Medium grained (1-3 mm) | Main alteration: |
Strike/Dip: | Direction: | |||
Plunge: |
Stratigraphic classification of host rock |
Era: | Proterozoic | Period: | Mesoproterozoic |
Province: | South Norwegian Basement Province | |
Geotec.unit: | Agder Complex | |
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Feldspar | Subordinate mineral (1-10%) | |
Ore mineral | Molybdenite | Major mineral (>10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Granite | Intrusive Original rock :Granite |
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Metamorphic facies :Amphibolite |
Information(s) in free text format |
Free text |
Jelå gruve ligger på nordsida av en kløft ca. 20-30 m lavere i terrenget (770-780 moh) enn en sti som fører fra hyttefeltet og nordover opp langs Geiteryggen. To stoller er anlagt mot nord fra kløfta. Den øverste fører inn til et større bergrom og er ikke tilgjengelig, men 10-15 m under denne er det drevet en stoll med retning 76°. Ved inngangen i sør er en finkornet dolerittgang som følger kløfta og er ca. 15 m bred. I stollen finnes både grå og rødlig porfyrisk granitt. Molybdenglans finnes i en pegmatittisk, 10 cm tykk kvartsgang i den porfyriske granitten og disseminert i grå granitt. Mektigheten til malmsonen er beskrevet å være ca. 10 m med jevn gehalt på 0,23 % MoS2 (Holmsen 1961). En stoll skal være drevet fra Ørnehommen gruve og inn under Jelå gruve og Bugge (1963) omtaler disse gruvene samlet. |
Bibliography: |
From NGU's Reference Archive: |
Bugge, Arne , 1963 |
Norges molybdenforekomster. |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.217;1-134 pages |
Abstract: | |
The ore fields and individual deposits which are mentioned in the text are shown on the map, figure 2. For those areas where the deposits lie so close together that they cannot be shown separately on this map, detail maps have been drawn on larger scales. In the descriptions there will also be found special maps covering the most important molybdenum areas. An index of the deposits which are mentioned is arranged both alphabetically and according to the numbers on the map. The majority, including the most important, of the ore deposits in Southern Norway lie within a marked zone, which is shown on the map, figure 3. At varying periods of time different metals have characterised the long zone of ore deposits: titanium in the southwest, then molybdenum in the area from Gursli to Knaben, copper and molybdenum in Telemark, silver, zinc and lead from Kongsberg eastwards, and further to the east, molybdenum again. From the map, figure 4, it can be seen that the most important groups of deposits are situated to both sides of the granite-gneiss area of the mountanious region of Southern Norway and that they lie in migmatised gneisses along the southwest side and in the schists and quartzites of the Telemark supracrustal suite along the northeast side. |
Holmsen, T. W. , 1961 |
Rapport over molybdenglansforekomster i Vestlandske distrikt i området Vest-Agder fylke samt herredene Lund og Sokndal i Rogaland. |
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 7513;178 pages |
Abstract: | |
Rapporten er ordnet i tre deler. Del 1 gir oversikt over alle mutede skjerp i området (side 4-106). Del 2 gir driftsberetninger hentet fra Norges Bergverksdrift for de skjerp hvor det har vært undersøkelsesarbeid eller regulær drift (side 107-135). Del 3 gir tittel med korte sammendrag av rapporter fra de aktuelle steder som er beskrevet (side 136-158). Side 158-176 består av kartbilag i M 1:50 000. Tittel forts.: ... Rogaland fylke. |
Müller, Axel; Henderson, Iain; Jourdan, Charles; Slagstad, Trond , 2016 |
Mineralization styles and formation temperatures of the Knaben molybdenum deposits, southern Norway |
;Norges geologiske undersøkelse;RAPPORT;NGU-rapport; No.2015.030;59 pages |
Abstract: | |
The report documents the lithologies and molybdenite mineralization exposed in underground mines of the Knaben molybdenum (Mo) mining district in Kvinesdal, Vest-Agder, SW Norway. Scanning electron microscope cathodoluminescence (SEM-CL) and trace element analyses of quartz by laser ablation inductively coupled mass Spectrometry (LA-ICP-MS) were performed on 37 quartz and quartz-bearing samples in order to better understand the P-T conditions during magma emplacement and Mo-mineralization. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
JS-W2121 | Dump |
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JS-W2122 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Ruben gruve |
(Object Id: 38441 28,01,00) |
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Location |
County: | Municipality: | Mangler () |
Map 1:50000: | Fjotland (1412-3) | Map 1:250000: | Mandal |
County: | UTM-Zone 33 - EUREF89/WGS84 |
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Resource |
Resource Type: | Ferroalloys (Cr,Ni,Co,V,Mo,W) | Resource Subtype: | Molybdenium | |
Element(s): | Mo |
Resources and production |
Activity: | Test mining | Reserves: | ||
Operating method: | Underground mining | Historical production: |
Information(s) in free text format |
Free text |
Ruben gruve er drevet på samme nivå som øvre stoll i Jelå gruve på sørsida av kløften. Ved befaring i juni 2021 var gruva fylt med snø og ikke tilgjengelig. |
The fact sheet was created on 08.05.2024 |
Copyright © 2024 Geological Survey of Norway |