Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 1554 - 001 Vassdalsvatnet | |||||
(Object Id: 4600) (Last updated: 27.01.2023) |
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Location |
County: | Møre og Romsdal | Municipality: | Averøy (1554) |
Map 1:50000: | Eide (1320-4) | Map 1:250000: | Ålesund |
Coordinate system: | EU89-UTM Zone 32 |
East: | 424510 m. | North: | 6984318 m. |
Longitude: | 7.5105330 | Latitude: | 62.9807530 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Kis Cu |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Resources and production |
Activity: | Test mining | Reserves: | ||
Operating method: | Underground mining | Historical production: |
Mineralization |
Genesis: | Volcex | Form: | Lens | |
Main texture: | Structureless | Min. distribution: | Semi-massive (20-50 % ore minerals) |
Main grain size: | Medium grained (1-3 mm) | Main alteration: |
Strike/Dip: | 225 / 40 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Period: |
Province: | ||
Geotec.unit: | ||
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Amphibole | Major mineral (>10%) | |
Gangue mineral | Quartz | Subordinate mineral (1-10%) | |
Gangue mineral | Garnet | Subordinate mineral (1-10%) | |
Gangue mineral | Feldspar | Subordinate mineral (1-10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Amphibolite | Extrusive Original rock :Basalt |
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Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Foliation | Strike/Dip :225 / 40 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Forekomsten ligger i lia sørøst for Vassdalsvatnet som er neddemt og vannkilden til Kårvåg-området og øyene utenfor. En bomvei fører opp til nordenden av vannet, og en sti kan følges på østsida av vannet. Forekomsten ligger i en mindre knaus og en vannfylt stoll som har retning 155° og er ca. 20 m lang er drevet. Ved inngangen dominerer grovkornet, granatrik amfibolitt og kun svake sulfidmineraliseringer kan sees. I en dagskjæring ovenfor stollen er det en ca. 1 meter mektig sulfidsone med disseminert magnetkis i amfibolitten. Blokker med massiv til semimassiv magnetkis med mindre mengder kobberkis er prøvetatt fra tippen som har et volum på ca. 80 m3. |
Bibliography: |
References not to be found in NGU's Reference Archive.: |
Wulff, P. 2010. Norrbotten Exploration AB’s exploration in West-Norway between Trondheim and Stavanger, 2010. BV Report 10097, 50 pp. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
JS-MR2206 | Dump |
|
NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Vassdalsvatnet SV |
(Object Id: 38777 1,01,00) |
|
Location |
County: | Møre og Romsdal | Municipality: | Averøy (1554) |
Map 1:50000: | Eide (1320-4) | Map 1:250000: | Ålesund |
Coordinate system: | EU89-UTM Zone 32 |
East: | 424423 m. | North: | 6984258 m. |
Longitude: | 7.5088450 | Latitude: | 62.9801880 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Kis Cu |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Amphibole | Major mineral (>10%) | |
Gangue mineral | Quartz | Subordinate mineral (1-10%) | |
Gangue mineral | Garnet | Subordinate mineral (1-10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Amphibolite | Extrusive Original rock :Basalt |
|
Metamorphic facies :Amphibolite |
Information(s) in free text format |
Free text |
Skjerpet ligger ca. 100 m sørvest for hovedforekomsten i en knaus hvor det er sprengt i en 2-3 m mektig sulfidsone i dels granatførende amfibolitt. Mineraliseringen er av samme type som i hovedforekomsten og en prøve med massiv magnetkis+kobberkis er tatt fra store blokker i tippen som er spredt nedenfor skjerpet. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
JS-MR2207 | Dump |
|
NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 1554 - 001 Vassdalsvatnet |
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# |
JS-MR2206 | Dump | 290 | 246 | 38 | 43 | 179 | .7 | 13.0 |
JS-MR2207 | Dump | 362 | 273 | 19 | 37 | 154 | .7 | 11.0 |
------------------ |
Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* |
JS-MR2206 | -5.0 | 22.0 | 4 | .8 | 180 | 14.55 | 2 | -0 | 0 |
JS-MR2207 | -5.0 | 15.0 | 2 | 1.1 | 290 | 16.85 | 1 | -0 | 0 |
------------------ |
Sample No. | Se* | Ga* | Ge* | In* | S% | V* | Cr* | Mn* | Fe% |
JS-MR2206 | 5.00 | 6.45 | 0.33 | 0.08 | 13.85 | 117 | 56 | 7060 | 35.40 |
JS-MR2207 | 6.00 | 7.20 | 0.23 | 0.08 | 12.20 | 161 | 65 | 3930 | 34.00 |
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Sample No. | Th* | U* | W* | Rb* | Sr* | Y* | Zr* | Nb* | Ta* |
JS-MR2206 | 3.55 | 4.30 | -0 | 11.7 | 69.0 | 25.8 | 47 | 3.90 | 0.28 |
JS-MR2207 | 2.42 | 5.20 | -0 | 19.9 | 71.3 | 30.1 | 41 | 3.90 | 0.29 |
------------------ |
Sample No. | Cs* | La* | Ce* | Li* | Be* | P* | Sc* | Te* | Hf* |
JS-MR2206 | 4.16 | 19.80 | 32.40 | 4 | 1 | 1200 | 5.70 | 0.84 | 1.20 |
JS-MR2207 | 3.06 | 13.30 | 21.30 | 7 | 2 | 1590 | 5.10 | 0.41 | 1.10 |
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Sample No. | Re* | Tl* | |||||||
JS-MR2206 | 19 | 0 | |||||||
JS-MR2207 | 24 | 1 |
The fact sheet was created on 02.05.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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