Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 5622 - 011 Tupajærvi | |||||
(Object Id: 709) (Last updated: 25.10.2005) |
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Location |
County: | Finnmark | Municipality: | Porsanger (5622) |
Map 1:50000: | Skoganvarre (2034-4) | Map 1:250000: | Karasjok |
Coordinate system: | EU89-UTM Zone 35 |
East: | 430107 m. | North: | 7760755 m. |
Longitude: | 25.1735810 | Latitude: | 69.9447270 |
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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: | Little Importance (reg. 18.02.2015) |
Resources and production |
Activity: | Test mining | Reserves: | ||
Operating method: | Underground mining | Historical production: | ,03 thousand tons |
Mineralization |
Genesis: | Volcex | Form: | Layer | |
Main texture: | Banded | Min. distribution: | Semi-massive (20-50 % ore minerals) |
Main grain size: | Medium grained (1-3 mm) | Main alteration: | Carbonatisation |
Strike/Dip: | 120 / 30 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Proterozoic | Period: | Paleoproterozoic |
Province: | Troms-Finnmark Basement Province | |
Geotec.unit: | Karasjok Greenstone Belt | |
Tectonic complex: | ||
Igneous complex: |
Group: | Iddjajav'ri | Formation: | Bakkilvarri |
Mineralogy |
Relationship | Mineral | Amount | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Quartz-mica schist | Sedimentary Original rock :Siliceous rock |
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Metamorphic facies :Amphibolite | |||
Wall rock | Carbonate bearing mica schist | Sedimentary Original rock :Argillaceous sediment |
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Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Foliation | Strike/Dip :120 / 30 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Forekomsten er kjent som Tupajervi eller Stuevann-stollen og ligger like ved veien gjennom Porsangmoen skytefelt. Det er drevet en 20m lang stoll med korte tverrslag innerst til begge sider. Den ble undersøkt i detalj i 1967 (Juve 1968, Røsholt 1969). Forekomsten er muligens av samme type som "Algascåkka" FI0061. |
The fact sheet was created on 08.05.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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