Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 5021 - 018 Kongsvoll | |||||
(Object Id: 4309) (Last updated: 01.07.1998) |
Drill Cores: Kongsvoll |
|
Location |
County: | Trøndelag | Municipality: | Oppdal (5021) |
Map 1:50000: | Snøhetta (1519-4) | Map 1:250000: | Røros |
Coordinate system: | EU89-UTM Zone 32 |
East: | 531849 m. | North: | 6906360 m. |
Longitude: | 9.6138760 | Latitude: | 62.2875060 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Sulphides | |
Element(s): | Kis |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Operations |
From - To | Activity | Comments | |
1985 - 1985 | Geophysics | Company/Institution :Folldal Verk A/S | |
1997 - 1997 | Sampling | Company/Institution :NGU-Malmreg. |
Mineralization |
Genesis: | Volcex | Form: | ||
Main texture: | Banded | Min. distribution: | Massive (>50 % ore minerals) |
Main grain size: | Fine grained (< 1 mm) | Main alteration: | Chloritisation |
Strike/Dip: | 130 / 30 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Period: |
Province: | Caledonides | |
Geotec.unit: | Blåhø-Surna Nappe Complex | |
Tectonic complex: | Blåhø Nappe | |
Igneous complex: |
Group: | Blåhø | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Amphibole | Major mineral (>10%) | |
Gangue mineral | Biotite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Pyrite | Accessory mineral (<1%) | |
Ore mineral | Chalcopyrite | Accessory mineral (<1%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Amphibolite | Extrusive Original rock :Basalt |
|
Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Foliation | Strike/Dip :130 / 30 | Post-mineralisation ;...Effect :None |
Information(s) in free text format |
Description |
Mineraliseringen har utgående 25 m nord for et høydepunkt (1013 m.o.h.), og er undersøkt med et lite skjerp (5 m3 tipp). Det er ikke kjent når skjerping har foregått. I 1985 utførte Folldal Verk A/S elektromagnetiske (Turam) målinger over mineraliseringen. I tildels klorittisert, fin- til middelskornig og karbonatholdig amfibolskifer er det i skjerpet en 2.5 m mektig rustsone, bestående av grov- til middelskornig, lite foliert amfibolitt med magnetkis-disseminasjon og spor av svovelkis og kobberkis. Svovelkis og kobberkis opptrer overveiende langs kontaktene til få-cm-mektige kvartslinser. I rustsonen er det også et par dm-mektige lag av klorittisert amfibolskifer. I bunnen av rustsonen er det 20 cm massiv, finkornig magnetkis-mineralisering. Mineraliseringen kan pga. overdekning ikke følges i strøkretningen. |
Bibliography: |
From NGU's Reference Archive: |
Nilsen, Odd , 1978 |
Caledonian sulphide deposits and minor iron-formations from the southern Trondheim region, Norway. |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.340;35-85 + k pages |
Abstract: | |
Within the southern and central parts of the Trondheim region of the Norwegian Caledonides a great number of small, stratabound cupriferous pyrite deposits are confined to mafic metavolcanics of the Gula, Støren and Fundsjø Groups of the Lower Palaeozoic succession. The deposits occuring within, or in close contact with the metavolcanics are characterized by their association with minor manganiferous oxide/silicate iron-formations - better known as "vasskis" ore type - within the metamorphic low-grade areas. The iron-fprmations of the metamorphic higher grade terrains on the other hand, which are extensively developed within the Gula Group, are mostly of a pyrrhotitic sulphide/silicate type and sulphurization processes are thought to have played an important role during the metamorphism. The pyrite deposits occurring adjacent to the metavolcanics bear no relationship to the iron-formations. They are embedded in pelitic, often carbonaceous assemblages (Gula Group) or within tuffitic members of the volcanogene Støren Group, and they are thought to represent re-sedimented (reworked) deposits. The pyrite deposits display varying degree of metamorphic reconstitution and a tectonic control has apparently determined their disc- or ruler-shaped morphology. |
References not to be found in NGU's Reference Archive.: |
Elvebakk, H. & Lile, O.B. 1986: Elektromagnetiske målinger, Turam, Kongsvoll og Heimtjønnhø 1985. BV 4462. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0106.01 | Bedrock |
|
NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 5021 - 018 Kongsvoll |
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# |
ST0106.01 | Bedrock | 476 | 102 | 12 | 7 | 145 | .9 | 6.0 |
------------------ |
Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sb* | Bi* | S% |
ST0106.01 | 5.0 | 6.0 | 7 | 1.9 | 18 | 10.00 | -3 | 5 | 24.50 |
------------------ |
Sample No. | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* | La* |
ST0106.01 | 77 | 18 | 1211 | 44.07 | 8.00 | -8.00 | -2 | 37.0 | 7.00 |
------------------ |
Sample No. | B* | ||||||||
ST0106.01 | 12 |
The fact sheet was created on 03.05.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
Copyright © 2024 Geological Survey of Norway |