Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 5033 - 009 Våråviken | |||||
(Object Id: 4429) (Last updated: 07.11.2023) |
|
Location |
County: | Trøndelag | Municipality: | Tydal (5033) |
Map 1:50000: | Tydal (1721-3) | Map 1:250000: | Trondheim |
Coordinate system: | EU89-UTM Zone 32 |
East: | 634824 m. | North: | 6996896 m. |
Longitude: | 11.6692860 | Latitude: | 63.0763450 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Zinc | |
Element(s): | Zn Cu Pb Kis Co |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Resources and production |
Activity: | Test mining | Reserves: | ||
Operating method: | Open pit and underground mining | Historical production: |
Operations |
From - To | Activity | Comments | |
1822 - 1824 | Test mining | Company/Institution :Røros Kobberverk | |
1997 - 1997 | Sampling | Company/Institution :NGU |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Genesis: | Volcex | Form: | Lens | |
Main texture: | Structureless | Min. distribution: | Massive (>50 % ore minerals) |
Main grain size: | Fine grained (< 1 mm) | Main alteration: | Silicification |
Strike/Dip: | Direction: | |||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Ordovician |
Province: | Caledonides | |
Geotec.unit: | Trondheim Nappe Complex | |
Tectonic complex: | ||
Igneous complex: |
Group: | Kjølhaug | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Feldspar | Major mineral (>10%) | |
Gangue mineral | Biotite | Subordinate mineral (1-10%) | |
Ore mineral | Pyrite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Major mineral (>10%) | |
Ore mineral | Sphalerite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Galena | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Kvarts-biotitt bergart | Sedimentary Original rock :Greywacke |
|
Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Foliation | Strike/Dip :32 / 10 | Post-mineralisation ;...Effect :Modifies | |
Wall rock | Mineral lineation | Dir./Plunge :235 / 10 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Våråviken ligger ca. 400 m sørvest for Livollen i ei li sørvest for Gammelvollsjøen. Den ligger i et 5-10 år gammelt hogstfelt med relativt tett løvskog, men tippen og avrenning fra denne er relativt godt synlig. Røros kobberverk drev forsøksdrift på forekomsten i perioden 1822-24 for å skaffe svovelkis til smeltingen av Grønskardmalmen. Malmen er relativt rik, men har trolig liten utstrekning. En 3x10 m dagskjæring med retning 340° er utdrevet og i tillegg finnes en trolig grunn, vannfylt sjakt. Nedenfor gruva ligger en tipp på ca. 200 m3. Malmen er ikke blottet i gruva, men på tippen finnes ulike typer av rik malm; massiv magnetkis malm med varierende mengde sinkblende, blyglans og kobberkis dominerer (prøve 03). Sinkblende- (prøve 01) eller kobberkis-rik (prøve 04) magnetkis malm er også vanlig. Innholdet av bly og sølv er også relativt høyt. Båndet svovelkis-sinkblende malm (prøve 02) og breksje-type magnetkis malm med bergartsfragmenter (prøve 05) er underordnete malmtyper på tippen. Området omkring forekomsten er svært overdekket, men nord for denne finnes middelskornet gabbro. Bergarten i dagskjæringen er i hovedsak finkornet og kvartsrik med varierende innhold av biotitt og amfibol. Den kan ligne vertsbergarten til Grønskard- og Allergot-forekomstene og er trolig av sedimentær opprinnelse. Den tektonostratigarfiske plasseringen av forekomsten er usikker. |
Photo(s) from the Deposit area: |
|
Bibliography: |
From NGU's Reference Archive: |
Aasgaard, Gunnar , 1927 |
Gruber og skjerp i kisdraget Øvre Guldal-Tydal. |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.129;1-196 pages |
Abstract: | |
The occurences described in this paper form a connection between th mining districts around Røros to the south and those around Meråker to the north. The occurences lie in mountain regions partly above the forest line. The list on page 12 contains the names of all known occurrences of whatever size within the district considered. Pl. I is a geological outline map of the district, compiled from maps in the Norwegian Geological Survey. In a geological summary on pages 18-27 it is shown that no pyrite occurrences of economic importance so far have been found in an eastern zone along the Swedish boundary where the rocks consist of hard schist with sparagmites, and igneous rocks. Neither have such occurrences been found in a zone of "Stuedalsskifer" and an other zone of "Gulaskifer" towards west, both indicated on the map. The occurrences of pyrite are chiefly found in connection with fine grained, light green or gravish, partly feldspar bearing schist and in connection with green schists, mostly fine grained hornblende schists. All these zones of schist gnereally strike north and dip west. The pyrite bearing schist lie on both sildes of a large zone of igneous rocks extending from Kjølifjell in the south over Hyllingen and Melshogna to Fangen in the Meråker district in the north. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0227.01 | Dump |
|
||||
ST0227.02 | Dump |
|
||||
ST0227.03 | Dump |
|
||||
ST0227.04 | Dump |
|
||||
ST0227.05 | Dump |
|
||||
399890 | Dump |
|
||||
399891 | Dump |
|
||||
399892 | Dump |
|
||||
399893 | Dump |
|
||||
399894 | Dump |
|
||||
399895 | Dump |
|
NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 5033 - 009 Våråviken |
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# |
ST0227.01 | Dump | 10435 | 99999 | 33499 | 169 | 64 | 126.0 | 67.0 |
ST0227.02 | Dump | 14091 | 92119 | 20881 | 357 | 8 | 47.0 | 1192.0 |
ST0227.03 | Dump | 15387 | 90231 | 14922 | 127 | 98 | 49.0 | 73.0 |
ST0227.04 | Dump | 34361 | 55193 | 9717 | 59 | 40 | 39.0 | 1834.0 |
ST0227.05 | Dump | 5152 | 92450 | 19620 | 450 | 84 | 49.8 | 613.0 |
399890 | Dump | 30600 | 94200 | 20400 | 846 | 31 | 53.9 | 363.0 |
399891 | Dump | 11200 | 75800 | 5691 | 114 | 69 | 26.9 | 199.0 |
399892 | Dump | 13600 | 152700 | 39500 | 417 | 18 | 82.5 | 322.0 |
399893 | Dump | 16600 | 87200 | 25300 | 698 | 15 | 56.0 | 831.0 |
399894 | Dump | 5062 | 69700 | 19900 | 485 | 45 | 44.2 | 448.0 |
399895 | Dump | 5075 | 5445 | 1195 | 65 | 53 | 3.9 | 210.0 |
------------------ |
Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sb* | Bi* | S% |
ST0227.01 | 2.0 | 1.0 | 69 | 707.1 | 11 | 11.00 | 118 | 577 | 31.73 |
ST0227.02 | 1.0 | 2.0 | 453 | 248.4 | 3 | 14.00 | 99 | 192 | 45.79 |
ST0227.03 | 3.0 | 2.0 | 35 | 200.6 | 3 | 20.00 | 59 | 187 | 34.98 |
ST0227.04 | 1.0 | 2.0 | 104 | 130.5 | 95 | 16.00 | 56 | 85 | 10.97 |
ST0227.05 | 2.0 | 2.0 | 519 | 244.7 | 2 | 19.00 | 126 | 210 | 36.85 |
399890 | 565 | 144.8 | 5 | 15.00 | 71 | 164 | |||
399891 | 82 | 96.9 | 3 | 1.00 | 28 | 82 | |||
399892 | 660 | 257.1 | 3 | 13.00 | 127 | 262 | |||
399893 | 776 | 144.3 | 3 | 10.00 | 208 | 207 | |||
399894 | 410 | 115.2 | 7 | 15.00 | 86 | 147 | |||
399895 | 109 | 12.1 | 109 | 1.00 | 11 | 8 |
------------------ |
Sample No. | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* | La* |
ST0227.01 | 10 | 5 | 1980 | 23.50 | 2.00 | -8.00 | -2 | 1.0 | 4.00 |
ST0227.02 | 4 | -1 | 619 | 17.63 | -2.00 | -8.00 | -2 | 11.0 | 1.00 |
ST0227.03 | -1 | -1 | 779 | 41.58 | 3.00 | -8.00 | -2 | -1.0 | -1.00 |
ST0227.04 | 100 | 99 | 901 | 14.71 | 10.00 | -8.00 | -2 | 5.0 | 29.00 |
ST0227.05 | 10 | 5 | 688 | 40.72 | 3.00 | -8.00 | -2 | 1.0 | 2.00 |
399890 | 10 | 74 | 496 | 38.19 | 3.0 | 0.50 | |||
399891 | 2 | 2 | 585 | 49.42 | 0.5 | 0.50 | |||
399892 | 3 | 106 | 527 | 32.26 | 4.0 | 0.50 | |||
399893 | 7 | 42 | 378 | 34.88 | 3.0 | 0.50 | |||
399894 | 14 | 39 | 492 | 42.88 | 3.0 | 1.00 | |||
399895 | 113 | 169 | 831 | 7.16 | 6.0 | 33.00 |
------------------ |
Sample No. | B* | Ti* | |||||||
ST0227.01 | -3 | ||||||||
ST0227.02 | 3 | ||||||||
ST0227.03 | 3 | ||||||||
ST0227.04 | -3 | ||||||||
ST0227.05 | -3 | ||||||||
399890 | 30 | ||||||||
399891 | 30 | ||||||||
399892 | 30 | ||||||||
399893 | 30 | ||||||||
399894 | 30 | ||||||||
399895 | 719 |
The fact sheet was created on 07.05.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
Copyright © 2024 Geological Survey of Norway |