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THE ORE DATABASE | |||||
Deposit Area 1943 - 064 | |||||
(Last updated 11.des.2023) |
Name of Deposit Area : Nihkevarri |
(Object Id : 1943,064,00,00) |
Location |
County : | Troms (19) | Municipality : | Kvænangen (1943) |
Map 1:50000: | Flintfjellet (1834-4) | Map 1:250000: | Nordreisa |
Marking point: | (Unavailable) |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Copper | |
Element(s): | Cu |
Production |
Activity: | Exploration | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: |
Importance |
Public: | (No data) |
Economical: | Not classified/evaluated |
Mineralization |
Era: | Proterozoic | Period: | Paleoproterozoic | |
Dating: | Method: | |||
Genesis: | Sedimentary deposit | Form: | Layer | |
Main texture: | Structureless | Min. distribution: | Disseminated (<20 % ore minerals) |
Main grain size: | Fine grained (< 1 mm) | Main alteration: |
Strike/Dip: | 170 / 85 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Proterozoic | Period: | Paleoproterozoic |
Province: | Caledonian Basement Province | |
Geotec.unit: | Alta-Kvænangen Greenstone Belt | |
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: | Storviknes |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Carbonate | Major mineral (>10%) | |
Gangue mineral | Quartz | Subordinate mineral (1-10%) | |
Ore mineral | Bornite | Major mineral (>10%) | |
Ore mineral | Covellite | Subordinate mineral (1-10%) | |
Ore mineral | Digenite | Subordinate mineral (1-10%) | |
Ore mineral | Chalcopyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Dolostone | Sedimentary Original rock :Dolomite |
|
Metamorphic facies :Greenschist | |||
Wall rock | Siltstone | Sedimentary Original rock :Siltstone |
|
Metamorphic facies :Greenschist |
Information(s) in free text format |
Free text |
Three layers of dolostone of the Storviknes Formation are exposed south of lake Nihkejavri. The central layer is about 25 m thick in the locality and comprises Cu-mineralisation in the lower (westernmost) part of the layer. Reddish, banded dolostone comprises quartz lenses and disseminations and veinlets of bornite and chalcopyrite over a thickness of ca. 0,5-1 m approximately one meter above the contact to the underlying greenish schistose siltstone. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
JS1408 | Bedrock |
|
NB! All analyse values are shown at the end of the printout.: |
Name of Locality : Nihkevarri nord |
(Object Id : 1943,064,01,00) |
Location |
County : | Troms (19) | Municipality : | Kvænangen (1943) |
Map 1:50000: | Flintfjellet (1834-4) | Map 1:250000: | Nordreisa |
Marking point: | Longitude: | 22.3251940 | Latitude: | 69.8009490 |
EU89-UTM Zone 34 | (Coordinates IS confirmed) |
X-coord: | 551063 m. | Y-coord: | 7744229 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Copper | |
Element(s): | Cu |
Production |
Activity: | Exploration | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: |
Information(s) in free text format |
Free text |
The central of three dolomite layers is 17-18 m thick in the locality. Massive and laminated to banded, locally strongly folded dolostone intercalated with thin siltstone bands comprises the lower part of this layer. The Cu-mineralisation occurs as disseminations of bornite and minor chalcocite and digenite in the lowermost, few dm-thick massive dolostone. The underlying greenish siltstone is more reddish along the contact to the dolostone. Only very weak disseminations of Cu-sulphides were observed in the lower (30-40 m thick, westernmost) and the upper dolostone layer (5 m thick, easternmost). |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
JS1405 | Bedrock |
|
||||
JS1406 | Bedrock |
|
NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 1943 - 064 Nihkevarri |
Element analyses |
( *=parts pr. million, #=parts pr.billion, Negative values means below detection limit value.) |
Sample No. | Sample Type | Cu* | Zn* | Pb* | Co* | Ni* | Ag* | Au# |
JS1405 | Bedrock | 8910 | 21 | 13 | 6 | 7 | 4.9 | 10.0 |
JS1406 | Bedrock | 4780 | 92 | 9 | 21 | 76 | 2.5 | 22.0 |
JS1408 | Bedrock | 127500 | 33 | 87 | 11 | 42 | 63.7 | 186.0 |
------------------ |
Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* |
JS1405 | -5.0 | -1.0 | 1 | .2 | 70 | 1.20 | -0 | 1 | 4 |
JS1406 | -5.0 | 1.0 | 1 | .1 | 160 | 40.80 | 0 | 1 | 4 |
JS1408 | -5.0 | -1.0 | 170 | 1.5 | 160 | 1.11 | 1 | 58 | 21 |
------------------ |
Sample No. | Se* | Ga* | Ge* | S% | V* | Cr* | Mn* | Fe% | Th* |
JS1405 | 1.00 | 0.85 | 0.07 | .21 | 6 | 5 | 4590 | .94 | 0.50 |
JS1406 | 1.00 | 8.83 | 0.12 | .10 | 64 | 70 | 1610 | 2.66 | 4.70 |
JS1408 | 2.00 | 3.36 | 0.08 | 3.90 | 20 | 28 | 1910 | 4.01 | 1.20 |
------------------ |
Sample No. | U* | W* | Rb* | Sr* | Y* | Zr* | Nb* | Ta* | Cs* |
JS1405 | 1.40 | 8 | 4.5 | 100.5 | 6.4 | 6 | 0.40 | -0.05 | 0.46 |
JS1406 | 10.70 | 1 | 35.7 | 167.0 | 14.8 | 65 | 2.50 | 0.20 | 6.81 |
JS1408 | 15.50 | 0 | 24.6 | 19.7 | 3.4 | 15 | 0.60 | 0.06 | 1.06 |
------------------ |
Sample No. | La* | Ce* | Li* | Be* | P* | Sc* | Ti* | Te* | Hf* |
JS1405 | 7.00 | 14.85 | 10 | 0 | 50 | 1.00 | 0 | -0.05 | 0.20 |
JS1406 | 25.00 | 56.40 | 53 | 0 | 420 | 8.70 | 0 | -0.05 | 1.90 |
JS1408 | 2.30 | 5.35 | 20 | 0 | 140 | 2.90 | 0 | 0.05 | 0.40 |
------------------ |
Sample No. | Re* | Tl* | |||||||
JS1405 | 2 | 0 | |||||||
JS1406 | 2 | 0 | |||||||
JS1408 | 2 | 0 |
The fact sheet was created on 15.05.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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