Norsk versjon | |||||
THE ???? DATABASE | |||||
Occurence 0 - 000 FEIL | |||||
(Object Id: ) (Last updated: 06.12.2023) |
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Location |
County: | Municipality: | Mangler () |
Map 1:50000: | Repparfjorden (1935-1) | Map 1:250000: | Honningsvåg |
County: | UTM-Zone 33 - EUREF89/WGS84 |
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Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Resources and production |
Activity: | Exploration | Reserves: | ||
Operating method: | Historical production: |
Mineralization |
Era: | Proterozoic | Period: | Paleoproterozoic | |
Genesis: | Hydrothermal vein | Form: | Plate | |
Main texture: | Vein network | Min. distribution: | Disseminated (<20 % ore minerals) |
Main grain size: | Medium grained (1-3 mm) | Main alteration: | Epidotisation |
Strike/Dip: | 13 / 70 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Proterozoic | Period: | Paleoproterozoic |
Province: | Caledonian Basement Province | |
Geotec.unit: | Komagfjord-Repparfjord Greenstone Belt | |
Tectonic complex: | Komagfjord window | |
Igneous complex: |
Group: | Saltvatn | Formation: | Ulveryggen |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Calcite | Major mineral (>10%) | |
Gangue mineral | Albite | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Major mineral (>10%) | |
Ore mineral | Pyrite | Subordinate mineral (1-10%) | |
Ore mineral | Hematite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Altered metagabbro | Intrusive Original rock :Gabbro |
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Metamorphic facies :Greenschist |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
HO-5-13 | Dump |
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HO-5-14 | Dump |
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HO-5-15 | Dump |
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HO-5-16 | Dump |
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JSVF_30 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
The fact sheet was created on 28.04.2024 |
Copyright © 2024 Geological Survey of Norway |