Fact Sheet for Deposit Area 2017

					Norsk versjon
	THE ORE DATABASE
	Deposit Area 2017 - 006
	(Last updated 08.nov.2021)

Name of Deposit Area : Ulveryggen

(Object Id : 2017,006,00,00)

Location

County :

Finnmark (20)

Municipality :

Kvalsund (2017)

Map 1:50000:

Repparfjorden (1935-1)

Map 1:250000:

Honningsvåg

Marking point:

Longitude:

24.2417440

Latitude:

70.4300560

EU89-UTM Zone 34

(Coordinates IS confirmed)

X-coord:

621137 m.

Y-coord:

7817063 m.

Commodity

	Main Type:	Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn)	Sub Type:	Copper
			Element(s):	Cu

Production

Activity:	Mining	Reserves:	8000 thousand tons
Prod. method:	Open pit mining	Production:	3100 thousand tons
Prod. status:	Disused, closed	Volume of dump:
		Resource estimat. standard:	JORC

Importance

Public: National Importance (reg. 27.06.2017)

Economical: Significant , (Confirmed 27.jun.2017 by Jan Sverre Sandstad)

Products

Element/product Crude ore grade or quality

CU .81 %

Ownership

Type of ownership Owner Land- and title number

Concessionary (Mining rights) Tore Birkeland - Metallica Mining

Operations

From - To Activity Comments

1903 - 1913 Pitting Company/Institution :Nordiska Grufaktiebolaget

1955 - 1963 Core drilling Company/Institution :Invex Corporation Ltd

1963 - 1970 Core drilling Company/Institution :A/S National Industri

1972 - 1979 Regular production Company/Institution :Folldal Verk A/S

Mineralization

Era: Proterozoic Period: Paleoproterozoic

Dating: Method:

Genesis: Sedex Form: Lens

Main texture: Pore space filling Min. distribution: Disseminated (<20 % ore minerals)

Main grain size: Medium grained (1-3 mm) Main alteration: No country rock alteration

Strike/Dip: Direction:

Plunge:

Stratigraphic classification of host rock

Era: Proterozoic Period: Paleoproterozoic

Province: Caledonian Basement Province

Geotec.unit: Komagfjord-Repparfjord Greenstone Belt

Tectonic complex:

Igneous complex:

Group: Saltvatn Formation: Ulveryggen

Mineralogy

Relationship Mineral Amount

Gangue mineral Quartz Major mineral (>10%)

Gangue mineral Feldspar Major mineral (>10%)

Gangue mineral Muscovite Subordinate mineral (1-10%)

Gangue mineral Chlorite Subordinate mineral (1-10%)

Gangue mineral Biotite Accessory mineral (<1%)

Gangue mineral Epidote Accessory mineral (<1%)

Ore mineral Hematite Major mineral (>10%)

Ore mineral Chalcocite Major mineral (>10%)

Ore mineral Chalcopyrite Major mineral (>10%)

Ore mineral Bornite Major mineral (>10%)

Ore mineral Pyrite Subordinate mineral (1-10%)

Ore mineral Magnetite Subordinate mineral (1-10%)

Ore mineral Malachite Accessory mineral (<1%)

Ore mineral Chromite Accessory mineral (<1%)

Ore mineral Covellite Accessory mineral (<1%)

Ore mineral Digenite Accessory mineral (<1%)

Ore mineral Ilmenite Accessory mineral (<1%)

Lithology:

Relationship Rock Origin

Host rock Conglomerate Sedimentary
Original rock :Conglomerate

Metamorphic facies :Greenschist

Host rock Sandstone Sedimentary
Original rock :Sandstone

Metamorphic facies :Greenschist

Information(s) in free text format

Free text

The Repparfjord copper deposit is located in sandstones on Ulveryggen in the Repparfjord-Komagfjord tectonic window. The Cu-mineralisations were discovered around 1900: In 1903 the Swedish company ‘Nordiska Grufaktiebolaget’ started to explore the area by trenching and digging minor adits. The area was abandoned until the Canadian company Invex Corporation Ltd continued exploration in 1955, before a Norwegian company acquired the rights in 1963. NGU carried out extensive investigations, including geological and geophysical mapping and core drilling, for A/S National Industri in the 1960’s. These investigations identified 10 Mt of ore with an average grade of 0.72 % Cu. Folldal Verk A/S acquired the rights to the deposit in 1970 and mined the deposit from May 1972 to June 1979. 3.1 Mt of ore with an average copper content of 0.663 were mined from four open pits. The copper concentrate of 51 000 t yielded 35.5 % Cu on average. The deposit is current (2008) under evaluation by the Norwegian company Wega Mining/Metallica Mining. The copper mineralisations are located in the lower part of the Ulverygg Formation, which is the lowermost part of the sedimentary Saltvatn Group. The Ulverygg Formation is at least 1000 m thick and consists of feldspathic and quartzitic sandstones and polymict conglomerates. Minor mafic intrusions are found the mining area. The ore zones consist of diffuse lenticular bodies along a strike length of 1.8 km with maximum thickness of 60-80 m in a northwesterly dipping limb of a NE-SW trending fold. The main ore minerals are chalcopyrite and bornite-chalcosite that occur mainly as disseminations and, to a lesser extent, along veinlets and cracks. The genesis of the mineralisations has been intensively discussed, with both syngenetic (during sedimentary or diagenetic processes) and epigenetic processes proposed. A structural control of at least part of the mineralisations is suggested. There is many similarities between the Repperfjord copper deposit and red bed copper deposits.

Photo(s) from the Deposit area:

Photo no. 1 showing Hovedfelt, NE-wall"

Photo no. 2 showing Hovedfelt, NE-wall"

Photo no. 3 showing Cu mineralisation in sandstone"

Bibliography:

From NGU's Reference Archive:

Hovland, R. , 1968

Rapparfjordfeltet: Geologisk oversiktskart og borhullsprofiler.

;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.808 B;2 pages

Abstract:

Rapporten har følgende tekst som innledning: "I de etterfølgende bilag finner man et oversiktskart over Cu- mineraliseringen med alle borhull inntegnet, samt en rekke borprofiler som viser årets borhull (1967) i vertikalsnitt. I flere av disse borprofilene har man fra tidligere sesonger borhull som også er inntegnet. " Borhullet S3, som ble boret ved Bratthammer grube, er ikke opptegnet da det ikke førte noen Cu - mineralisering. "I borprofilene er kobbergehalten avsatt grafisk langsetter borhullet, og det er videre skilt mellom ulike Cu - mineraliseringer og bergatstyper."

Hovland, Roar , 1969

Repparfjordfeltet.

;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.888;19 pages

Abstract:

Etter oppdrag fra A/S National Industri har Norges geologiske undersøkelse i årene 1964 - 1968 gjennomført undersøkelser av malmforekomstene i Repparfjord. Undersøkelsesprogrammet har omfattet geofysikk og geokjemisk prospektering, geologisk kartlegging og diamantboringer. Den geofysisk og geokjemiske pros- pekteringen samt diamantboringsprogrammet ble fullført i 1967. I sesongen 1968 har man undersøkt nærmere de geofysiske og geokjemiske anomalier som er frem- kommet utenfor selve malmfeltet samt fullført den geologiske kartleggingen av området. Et fremtidig malmletingsprogram vil naturlig falle i to deler. a) Å under- søke Ulverygg-malmens eventuelle fortsettelse videre øst, og vestover samt dens forløp mot dypet i Hovedfeltet. b) Å undersøke de påviste impregnasjonsområdene mellom Bratthammer og Stein- fjell samt å drive et videre arbeid vestover i kvartsittområdet. Likeledes kan det være aktuelt å se nærmere på forekomster i Porsafeltet.

Hovland, R. , 1966

Geologisk undersøkelse av Repparfjordfeltet sommeren 1965.

;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.693 B;15 pages

Abstract:

Rapporten har følgende innhold: - Prøvetaking: Nordfeltet, Hansfeltet, Hovedfeltet. - Mineraliseringssoner: 1. Soner med svovelkis og kobberkis. 2. Soner med kobberkis. 3. Soner med bornitt, kobberglans og neodigenitt. 4. Kvartsganger førende bornitt og kobberglans. 5. Ganger førende hematitt, bornitt og kvarts. - Konklusjon. - Plansjer 1 - 3 (fotos av planslip og stuffer). - Bilag 1 - 4: 1. Oversiktskart M: 1:10 000. 2. Cu - mineralisering ved "Hans" M: 1:1 000. 3. Geologi M: 1:2 500. 4. Blokkdiagram over en del av feltet M: 1:2 500.

Hovland, R. , 1968

Malmberegning av Repparfjordfeltet. (Ba nr. 4095) Bilagsbind. (Ba nr. 4094)

;Norges geologiske undersøkelse;RAPPORT;NGU-rapport; No.808 C;54 pages

Abstract:

Rapporten foreligger i to bind. Bind I består av kommentarer og analyselister for forekomstene Vestfeltet, Hovedfeltet, Østfeltet - John, Østfeltet - Erik, Østfeltet - Nord, Dypmalmen og Hansfeltet, etterfulgt av fem plansjer med tonnasje / gehaltberegninger for hver av forekomstene, Beregningene bygger på resultatene fra 9842 m. diamantboringer (480 m. i 1909, 2358 m. i 1957 og 7004 m. i 1965 - 1967), 1720 m. røskegrøfter og 760 m. underjordsdrifter (begge de siste fra 1904 - 1909). Bind II består av syv tegninger med plankart og profiler som viser registrerte Cu - verdier i dagen og i borhull for hver av forekomstene.

Paulsen, P.; Hovland, R. , 1968

Repparfjordfeltet: Rapport over undersøkelser 1967.

;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.808;16 pages

Abstract:

Rapporten har følgende innholdsfortegnelse: - Sammendrag. - Innledning. - Utførte arbeider i 1967. - Geologi - Malmforekomster. - Resultater. - Malmberegning. - Avbygging av forekomstene i Repparfjord. - Kalkyle for anlegg og drift. - Konklusjon. - Forslag til feltarbeider i 1968. - Oversikt over diamantborhull boret i 1967. - Fortegnelse over underrapporter vedrørende malmundersøkelsene i 1967. - Bilag: 1. Geologisk oversiktskart M: 1:10 000. 2. Oversiktskart over borhull og mineraliseringssoner M: 1:5 000. 3. Blokkdiagram over Ulveryggfeltet M: 1:5 000. 4. Borprofil 10160Y M: 1:1 000. 5. Forslag til plassering av anleggene M: 1:10 000.

Sandstad, Jan Sverre ; Viola, Giulio ; Nilsson, Lars Petter , 2007

Reconnaissance structural geological mapping and field XRF-analyses of the Ulveryggen copper deposit, Finnmark, Norway.

;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.2007.064;16 s. pages

Abstract:

Reconnaissance structural geological mapping and field XRF-analyses with a portable XRF-analyzer were carried out at the now closed Ulveryggen copper mine, Repparfjord Window, Finnmark. The goals of the study were to better understand the structural setting of the mineralisations at Ulveryggen and to test a handheld XRF-analyzer on this type of copper deposit. Preliminary conclusions suggest a structural control of at least part of the mineralisations. Suggestions for further studies include a helicopter-borne geophysical survey, meso-scale structural geological mapping and detailed studies of mineralisations and micro-structures.

Reitan, Paul H. , 1963

The geology of the Komagfjord tectonic window of the Raipas suite, Finnmark, Norway.

;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.221;1-71 + kar pages

Abstract:

The report is based on four summers (1956-59) of field work in an area of approximately 860 km2. The area is located in western Finnmark, northern Norway, between 70 degrees 10' and 70 degrees 31' N latitude and 12 degrees 40' and 13 degrees 50' E Oslo longitude. The purpose of the investigation was to study the rocks within a hitherto mainly unexamined area of Precambrian rocks surrounded by Caledonian rocks. Portions of the area near the sea had been visited by a few geologists prior to the initiation of this investigation. It was therefor quite certain that the rocks were Precambrian in age and constituted a window in the Caledonides, but the size of the window was unknown nor had most of the window been studied geologically. This report establishes the Precambrian age of the rocks and delineates the boundaries of the window. The Precambrian rocks along the western coast of Finnmark were previously called the Raipas formation and known to outcrop in (at least) two windows. As this report differentiates seven formations which constitute two groups whithin the Komagfjord (the northernmost) tectonic window, it is purposed that the Precambrian rocks of the two windows be known as the Raipas suite.

Pharaoh, Tim C.; Ramsey, Donald; Jansen, Øystein , 1983

Stratigraphy and structure of the northern part of the Repparfjord - Komagfjord window, Finnmark, Northern Norway.

;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.377;1-45 pages

Abstract:

In the northern district of the Repparfjord-Komagfjord Window, supracrustal and intrusive rocks of Early Proterozoic age are unconformably overlain by a thin sequence of Vendian sediments. Both of these units are overthrust by allochthonous rocks of the lavas, tuffs and sediments of the Raipas Supergroup and intrusions of the Raudfjell Suite, regionally metamorphosed at greenschist facies during the polyphase Svecokarelian Orogeny, c. 1840 Ma. The c. 8 km thick supracrustal sequence is divided into four groups and eleven formations on a lithostratigraphic basis. The lithological characteristics of these units are described and compared with rocks of similiar age elsewhere in N. Norway. The stratigraphy and sedimentology of the thin (<200 m thick), autochtonous, Vendian cover sequence is also described. The caledonian Orogeny resulted in complex deformation of the autochtonous cover as well as considerable reactiviation of the underlying basement.

Bjørlykke, Arne; Olerud, Svein; Sandstad, Jan Sverre , 1985

Metallogeny of Finnmark, North Norway

;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU Bulletin; No.403;183-196 pages

Abstract:

Metalliferous ore deposits and mineralisations in the county of Finnmark occur in rocks ascribed to three specific periods of geological time: 1) Archaean 2) Early Proterozoic 3) Caledonian. The only Archaean ore deposits is located at the largest iron mine in Norway, Sydvaranger; this was deposited in a shelf environment. The Early Proterozoic volcano-sedimentary belts can be divided into three major metallogenetic provinces. In the easternmost Pasvik area no significant deposits are known and only a few minor nickel mineralisations are present. The rocks of the Karasjok Greenstone Belt are thought to have accumulated during a complete "Wilson orogenic cycle" and contain both stratiform and stratabound copper deposits, banded iron formations and nickel mineralisations. A continental rifting model is more likely for the rocks of the Kautokeino Greenstone Belt and for correlative units in the tectonic windows to the northeast. Stratabound copper deposits are dominant, occurring in both metavolcanites and metasediments, but gold, uranium and REE minerali- sations are also found. This province includes the second operating ore mine in Finnmark at present, the Bidjovagge copper-gold mine. The Caledonian province contains lead deposits in both amphibolite-facies and very low grade metasandstones and Fe-Ti occurrences in mafic and ultramafic intrusive bodies in the Seiland magmatic province.

References not to be found in NGU's Reference Archive.:

Stribrny, B. 1985: The Conglomerate-hosted Repparfjord Copper Ore Deposit, Finnmark, Norway. Monograph Series on Mineral Deposits, Berlin-Stuttgart, 24, 75pp.

Sandstad, J.S. 1986: The Repparfjord copper deposit. In Sandstad, J.S. (ed.): Proterozoic copper mineralizations in Northernmost Norway. SGU Ser. Ca nr.64, 7-9.

Fabricius, J. 1979: Kobberforekomsten på Ulveryggen, Finnmark, Norge. Dansk geol. Forening, Årsskrift for 1979, p. 107-110.

Fieldsamples

Sample No. Sample type Miscellanrous

HO-2-10 Bedrock

Sampler :Ihlen, P.M./...Stored :Løkken

Comment :Grå sandstein med tynne (1-2mm) konkordante striper av kobberkis og svovelkis? Spredte kobberglanskorn i sandsteinen.

No. of registrated element analyses = 1

HO-2-11 Bedrock

Sampler :Ihlen, P.M./...Stored :Løkken

Comment :Kvartsganger som fører grovkornete aggregater av kobberkis, bornitt og tildels kloritt-aktinolitt. Gangene gjennomsetter kobberkis-rik sandstein.

No. of registrated element analyses = 1

HO-2-12 Bedrock

Sampler :Ihlen, P.M./...Stored :løkken

Comment :Grå kryss-sjiktet sandstein med rik disseminasjon og tynne sprekkefyllinger av kobberkis.

No. of registrated element analyses = 1

HO-2-7 Bedrock

Sampler :Ihlen, P.M./...Stored :Løkken

Comment :Grov kvartsbollet sandstein med spredte kobberglanskorn.

No. of registrated element analyses = 1

HO-2-8 Bedrock

Sampler :Ihlen, P.M./...Stored :Løkken

Comment :5mm brede kvartsårer med kobberkis og bornittaggregater. Årene gjennomsetter grovkornet sandstein.

No. of registrated element analyses = 1

HO-2-9 Bedrock

Sampler :Ihlen, P.M./...Stored :Løkken

Comment :Kobberkis disseminasjon og større enkelte aggregater av kobberkis langs kobberkis-bornitt fylte sprekker i sandstein.

No. of registrated element analyses = 1

NB! All analyse values are shown at the end of the printout.:

Name of Sample point : Repparfjord

(Object Id : 2017,006,00,01)

Location

County : Finnmark (20) Municipality : Kvalsund (2017)

Map 1:50000: Repparfjorden (1935-1) Map 1:250000: Honningsvåg

Marking point: Longitude: 24.2374190 Latitude: 70.4294520

EU89-UTM Zone 34 (Coordinates IS confirmed)

X-coord: 620980 m. Y-coord: 7816987 m.

Commodity

Main Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Sub Type: Copper

Element(s): Cu

Fieldsamples

Sample No. Sample type Miscellanrous

HO-2-105 Bedrock

Sampler :Sandstad, J.S./...Stored :Løkken

Comment :Sandstein, grovkornet, kvarts rik, grågrønn med svak disseminasjon av kobberglans.

No. of registrated element analyses = 1

HO-2-106 Bedrock

Sampler :Sandstad, J.S./...Stored :Løkken

Comment :Sandstone, finkornet, svakt skifrig, noe disseminasjon av kobberglans.

No. of registrated element analyses = 1

HO-2-107 Bedrock

Sampler :Sandstad, J.S./...Stored :Løkken

Comment :Sandstein, finkornet, grå med svak kobberkis disseminasjon.

No. of registrated element analyses = 1

HO-2-108 Bedrock

Sampler :Sandstad, J.S./...Stored :Løkkken

Comment :Sandstein, fin- til svært finkornet, svakt skifrig med svak kobberglans disseminasjon.

No. of registrated element analyses = 1

HO-2-109 Bedrock

Sampler :Sandstad, J.S./...Stored :Løkken

Comment :Sediment/"porphyritic pipe", finkornet, mørk grågrønn noen kvartsboller og mørkere grønne flekkker, svak pyritt disseminasjon.

No. of registrated element analyses = 1

NB! All analyse values are shown at the end of the printout.:

Name of Sample point : Repparfjord

(Object Id : 2017,006,00,02)

Location

County : Finnmark (20) Municipality : Kvalsund (2017)

Map 1:50000: Repparfjorden (1935-1) Map 1:250000: Honningsvåg

Marking point: Longitude: 24.2444650 Latitude: 70.4306180

EU89-UTM Zone 34 (Coordinates IS confirmed)

X-coord: 621236 m. Y-coord: 7817131 m.

Commodity

Main Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Sub Type: Copper

Element(s): Cu

Fieldsamples

Sample No. Sample type Miscellanrous

HO-1-100 Bedrock

Sampler :Sandstad, J.S./...Stored :Løkken

Comment :Sandstein, fin- til middelskornet med relativt rik kobberglans disseminasjon.

No. of registrated element analyses = 1

HO-1-101 Bedrock

Sampler :Sandstad, J.S./...Stored :Løkken

Comment :Sandstone, fin- til middels kornet, gråhvit med noe disseminasjon av kobberkis og bornitt.

No. of registrated element analyses = 1

HO-1-102 Bedrock

Sampler :Sandstad, J.S./...Stored :Løkken

Comment :Sandstein, grusig/konglomeratisk, 1-2 cm rundete kvarts/kvartsitt boller, grå matriks som er rik på kobberglans.

No. of registrated element analyses = 1

HO-1-103 Bedrock

Sampler :Sandstad, J.S./...Stored :Løkken

Comment :Kvartsgang, grovkornet, grønnlig hvit med noe middelskornet kobberkis.

No. of registrated element analyses = 1

HO-1-104 Bedrock

Sampler :Sandstad, J.S./...Stored :Løkken

Comment :Sandstein, finkornet, mørk grå med noe disseminasjon av kobberkis.

No. of registrated element analyses = 1

NB! All analyse values are shown at the end of the printout.:

Name of Sample point : Repparfjord

(Object Id : 2017,006,00,03)

Location

County : Finnmark (20) Municipality : Kvalsund (2017)

Map 1:50000: Repparfjorden (1935-1) Map 1:250000: Honningsvåg

Marking point: Longitude: 24.2386520 Latitude: 70.4296020

EU89-UTM Zone 34 (Coordinates IS confirmed)

X-coord: 621025 m. Y-coord: 7817006 m.

Commodity

Main Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Sub Type: Copper

Element(s): Cu

Fieldsamples

Sample No. Sample type Miscellanrous

HO-1-1 Bedrock

Sampler :Ihlen, P.M.+/...Stored :Løkken

Comment :Lys grå skifrig sandstein med disseminasjon av kobberglans og litt bornitt.

No. of registrated element analyses = 1

HO-1-2 Bedrock

Sampler :Ihlen, P.M./...Stored :Løkken

Comment :Lys grå sandstein med gruslag dominert av kvartsboller. Fører finkornet disseminasjon av kobberkis i sandstein og opptil 5 mm store aggregater og årer av kobberkis i gruslag.

No. of registrated element analyses = 1

HO-1-3 Bedrock

Sampler :Ihlen, P.M./...Stored :Løkken

Comment :Skifrig grønnlig grå sandstein med rik kobberkis disseminasjon. Enkelte tynne grovklastiske lag i sandsteinen.

No. of registrated element analyses = 1

HO-1-4 Bedrock

Sampler :Ihlen, P.M./...Stored :Løkken

Comment :Gruslag i sandstein med fin til middelskornet kobberkis disseminert. Enkelte mm brede kobberkis årer og cm store aggregater.

No. of registrated element analyses = 1

HO-1-5 Bedrock

Sampler :Ihlen, P.M./...Stored :Løkken

Comment :Finkornet kobberkis disseminasjon i grålig og svart skifrig sandstein.

No. of registrated element analyses = 1

HO-1-6 Bedrock

Sampler :Ihlen, P.M./...Stored :Løkken

Comment :Sterkt skifrig grønnlig sandstein med malakittbelegg på skifrighetsplan og korngrenser.

No. of registrated element analyses = 1

NB! All analyse values are shown at the end of the printout.:

Name of Locality : Hans gruve

(Object Id : 2017,006,01,00)

Location

County : Finnmark (20) Municipality : Kvalsund (2017)

Map 1:50000: Repparfjorden (1935-1) Map 1:250000: Honningsvåg

Marking point: Longitude: 24.2771500 Latitude: 70.4356510

EU89-UTM Zone 34 (Coordinates IS confirmed)

X-coord: 622426 m. Y-coord: 7817757 m.

Commodity

Main Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Sub Type: Copper

Element(s): Cu

Production

Activity: Test mining Reserves:

Prod. method: Underground mining Production:

Prod. status: Disused, closed Volume of dump:

Structures

Location: Type: Orientation(360 gr.): Relation to min.:

Host rock Primary layering Strike/Dip :63 / 55 Pre-mineralisation ;...Effect :Controls

Fieldsamples

Sample No. Sample type Miscellanrous

HO-3-110 Bedrock

Sampler :Sandstad, J.S./...Stored :løkken

Comment :Sandstein, gråhvit, kvarts rik, noe disseminasjon av kobberkis i aggregater og langs stikk, kraftigere deformert bergart.

No. of registrated element analyses = 1

HO-3-111 Bedrock

Sampler :Sandstad, J.S./...Stored :Løkken

Comment :Sandstein, gråhvit, kvartsårer med bornitt omkring og svak disseminasjon av kobberkis.

No. of registrated element analyses = 1

HO-3-112 Bedrock

Sampler :Sandstad, J.S./...Stored :Løkken

Comment :Sandstein, grågrønn, middelskornet med noe disseminasjon av bornitt og kobberkis (30 cm mektig lag).

No. of registrated element analyses = 1

NB! All analyse values are shown at the end of the printout.:

Name of Locality : Vestbruddet

(Object Id : 2017,006,02,00)

Location

County : Finnmark (20) Municipality : Kvalsund (2017)

Map 1:50000: Repparfjorden (1935-1) Map 1:250000: Honningsvåg

Marking point: (No coordinates)

Commodity

Main Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Sub Type: Copper

Element(s): Cu

Production

Activity: Mining Reserves:

Prod. method: Open pit mining Production:

Prod. status: Disused, closed Volume of dump:

Photo(s) from the Deposit area:

Photo no. 1 showing Sandstone with Cu mineralisation"

Photo no. 2 showing Vestfelt, looking towards NE"

Photo no. 3 showing Vestfelt, looking towards SW"

Name of Locality : Erik

(Object Id : 2017,006,03,00)

Location

County : Finnmark (20) Municipality : Kvalsund (2017)

Map 1:50000: Repparfjorden (1935-1) Map 1:250000: Honningsvåg

Marking point: (No coordinates)

Commodity

Main Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Sub Type: Copper

Element(s): Cu

Production

Activity: Mining Reserves:

Prod. method: Open pit mining Production:

Prod. status: Disused, closed Volume of dump:

Name of Locality : John

(Object Id : 2017,006,04,00)

Location

County : Finnmark (20) Municipality : Kvalsund (2017)

Map 1:50000: Repparfjorden (1935-1) Map 1:250000: Honningsvåg

Marking point: (No coordinates)

Commodity

Main Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Sub Type: Copper

Element(s): Cu

Production

Activity: Mining Reserves:

Prod. method: Open pit mining Production:

Prod. status: Disused, closed Volume of dump:

Analyse Results

from

Deposit Area 2017 - 006 Ulveryggen

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#

HO-1-1 Bedrock 16970 17 6 1 9 3.8 3.0

HO-1-100 Bedrock 47903 1 3 4 8 6.4 19.0

HO-1-101 Bedrock 16746 1 6 4 9 1.8 14.0

HO-1-102 Bedrock 36772 1 6 13 35 3.7 6.0

HO-1-103 Bedrock 29779 1 2 15 63 4.9 9.0

HO-1-104 Bedrock 47981 1 5 7 22 7.4 13.0

HO-1-2 Bedrock 5931 65 3 3 14 .7 4.0

HO-1-3 Bedrock 3203 12 3 1 21 .1 10.0

HO-1-4 Bedrock 4515 12 3 1 27 .2 3.0

HO-1-5 Bedrock 12441 3 2 7 32 2.6 9.0

HO-1-6 Bedrock 12702 1 5 1 14 5.0 10.0

HO-2-10 Bedrock 22477 1 2 8 30 4.3 12.0

HO-2-105 Bedrock 94 5 3 6 29 .1 1.0

HO-2-106 Bedrock 10740 1 2 7 34 1.8 16.0

HO-2-107 Bedrock 5149 5 3 7 38 .6 3.0

HO-2-108 Bedrock 262 8 2 6 29 .1 1.0

HO-2-109 Bedrock 611 53 6 25 145 .2 1.0

HO-2-11 Bedrock 32413 1 4 7 26 4.8 36.0

HO-2-12 Bedrock 10525 4 2 7 32 .5 34.0

HO-2-7 Bedrock 5757 12 2 8 44 1.1 4.0

HO-2-8 Bedrock 5082 9 2 7 39 1.2 2.0

HO-2-9 Bedrock 7799 9 2 8 42 1.7 3.0

HO-3-110 Bedrock 3047 4 6 8 41 .5 9.0

HO-3-111 Bedrock 1238 3 2 4 28 1.1 3.0

HO-3-112 Bedrock 35954 1 7 10 27 17.9 83.0

------------------

Sample No. Pt# Pd# Rh# As* Cd* Ba* Mo* Sb* Bi*

HO-1-1 1.0 2.0 2.0 2 1.0 80 3.00 3 7

HO-1-100 2.0 2.0 2.0 2 1.0 48 32.00 2 2

HO-1-101 2.0 2.0 2.0 2 1.0 22 60.00 2 2

HO-1-102 1.0 2.0 2.0 2 1.0 53 3.00 2 2

HO-1-103 2.0 2.0 2.0 3 1.0 57 10.00 2 2

HO-1-104 2.0 2.0 2.0 2 1.0 56 6.00 2 2

HO-1-2 1.0 2.0 2.0 3 1.0 53 5.00 2 2

HO-1-3 1.0 2.0 2.0 4 1.0 148 2.00 2 2

HO-1-4 2.0 2.0 2.0 3 1.0 90 2.00 2 2

HO-1-5 2.0 2.0 2.0 2 1.0 102 6.00 2 2

HO-1-6 1.0 2.0 2.0 2 1.0 134 9.00 2 8

HO-2-10 4.0 2.0 2.0 2 1.0 169 1.00 2 8

HO-2-105 2.0 2.0 2.0 2 1.0 36 2.00 2 2

HO-2-106 1.0 2.0 2.0 2 1.0 72 2.00 2 2

HO-2-107 2.0 2.0 2.0 2 1.0 87 2.00 2 2

HO-2-108 3.0 3.0 2.0 2 1.0 144 1.00 2 2

HO-2-109 2.0 5.0 2.0 3 1.0 79 2.00 2 4

HO-2-11 3.0 2.0 2.0 3 1.0 38 2.00 2 5

HO-2-12 4.0 2.0 2.0 5 1.0 132 1.00 4 2

HO-2-7 4.0 5.0 2.0 5 1.0 92 1.00 3 2

HO-2-8 1.0 2.0 2.0 2 1.0 110 2.00 2 8

HO-2-9 3.0 3.0 2.0 2 1.0 90 2.00 2 2

HO-3-110 1.0 2.0 2.0 2 1.0 427 2.00 2 2

HO-3-111 1.0 2.0 2.0 2 1.0 47 3.00 2 2

HO-3-112 2.0 2.0 2.0 2 1.0 75 3.00 2 19

------------------

Sample No. S% V* Cr* Mn* Fe% Th* U* W* Sr*

HO-1-1 .32 4 18 15 .50 4.00 5.00 1 5.0

HO-1-100 .99 3 14 16 .60 3.00 5.00 1 5.0

HO-1-101 .49 1 21 29 .79 2.00 5.00 1 4.0

HO-1-102 .67 11 100 91 1.61 6.00 5.00 1 3.0

HO-1-103 .66 23 116 120 3.11 9.00 5.00 1 9.0

HO-1-104 .96 8 29 36 1.35 4.00 5.00 1 3.0

HO-1-2 .54 5 35 28 1.26 7.00 5.00 1 4.0

HO-1-3 .28 11 29 38 1.23 5.00 5.00 1 2.0

HO-1-4 .29 8 43 65 1.66 4.00 5.00 1 5.0

HO-1-5 .29 9 39 68 1.24 3.00 5.00 1 4.0

HO-1-6 .15 6 15 23 .62 5.00 5.00 1 5.0

HO-2-10 .44 23 151 66 2.28 7.00 5.00 1 6.0

HO-2-105 .01 8 53 55 1.45 3.00 5.00 1 4.0

HO-2-106 .23 10 63 83 1.53 5.00 5.00 1 3.0

HO-2-107 .13 9 63 80 1.41 5.00 5.00 1 3.0

HO-2-108 .01 8 20 56 .87 7.00 5.00 1 4.0

HO-2-109 .01 46 400 445 3.94 4.00 5.00 1 4.0

HO-2-11 .99 12 87 77 1.60 5.00 5.00 1 9.0

HO-2-12 .89 15 100 93 2.27 4.00 5.00 1 5.0

HO-2-7 .12 13 111 91 1.81 11.00 5.00 1 6.0

HO-2-8 .12 12 93 83 1.86 5.00 5.00 1 6.0

HO-2-9 .22 15 124 91 1.96 16.00 5.00 1 5.0

HO-3-110 .14 14 56 61 2.78 3.00 5.00 1 5.0

HO-3-111 .03 6 36 51 .96 2.00 5.00 1 3.0

HO-3-112 .95 8 100 45 2.12 9.00 5.00 1 2.0

------------------

Sample No. La* B* Na* Mg* Al* P* K * Ca* Ti*

HO-1-1 7.00 4 0 0 0 0 0 0 0

HO-1-100 6.00 3 0 0 0 0 0 0 0

HO-1-101 6.00 2 0 0 0 0 0 0 0

HO-1-102 6.00 3 0 0 1 0 0 0 0

HO-1-103 13.00 2 0 1 1 0 0 0 0

HO-1-104 7.00 2 0 0 0 0 0 0 0

HO-1-2 6.00 2 0 0 0 0 0 0 0

HO-1-3 13.00 2 0 0 1 0 0 0 0

HO-1-4 8.00 3 0 0 1 0 0 0 0

HO-1-5 7.00 5 0 0 1 0 0 0 0

HO-1-6 8.00 2 0 0 0 0 0 0 0

HO-2-10 6.00 2 0 0 0 0 0 0 0

HO-2-105 5.00 2 0 0 0 0 0 0 0

HO-2-106 7.00 2 0 0 1 0 0 0 0

HO-2-107 9.00 2 0 0 1 0 0 0 0

HO-2-108 25.00 4 0 0 1 0 0 0 0

HO-2-109 6.00 3 0 3 3 0 0 0 0

HO-2-11 12.00 2 0 0 0 0 0 0 0

HO-2-12 6.00 2 0 0 0 0 0 0 0

HO-2-7 12.00 4 0 1 1 0 0 0 0

HO-2-8 12.00 2 0 0 1 0 0 0 0

HO-2-9 13.00 2 0 1 1 0 0 0 0

HO-3-110 8.00 2 0 0 0 0 0 0 0

HO-3-111 8.00 3 0 0 0 0 0 0 0

HO-3-112 8.00 2 0 0 0 0 0 0 0

	Type of ownership	Owner	Land- and title number
	Concessionary (Mining rights)	Tore Birkeland - Metallica Mining

From - To	Activity	Comments
1903 - 1913	Pitting	Company/Institution :Nordiska Grufaktiebolaget
1955 - 1963	Core drilling	Company/Institution :Invex Corporation Ltd
1963 - 1970	Core drilling	Company/Institution :A/S National Industri
1972 - 1979	Regular production	Company/Institution :Folldal Verk A/S

Era:	Proterozoic	Period:	Paleoproterozoic
Dating:		Method:
Genesis:	Sedex	Form:	Lens
Main texture:	Pore space filling	Min. distribution:	Disseminated (<20 % ore minerals)

	Province:	Caledonian Basement Province
	Geotec.unit:	Komagfjord-Repparfjord Greenstone Belt
	Tectonic complex:
	Igneous complex:

Relationship	Mineral	Amount
Gangue mineral	Quartz	Major mineral (>10%)
Gangue mineral	Feldspar	Major mineral (>10%)
Gangue mineral	Muscovite	Subordinate mineral (1-10%)
Gangue mineral	Chlorite	Subordinate mineral (1-10%)
Gangue mineral	Biotite	Accessory mineral (<1%)
Gangue mineral	Epidote	Accessory mineral (<1%)
Ore mineral	Hematite	Major mineral (>10%)
Ore mineral	Chalcocite	Major mineral (>10%)
Ore mineral	Chalcopyrite	Major mineral (>10%)
Ore mineral	Bornite	Major mineral (>10%)
Ore mineral	Pyrite	Subordinate mineral (1-10%)
Ore mineral	Magnetite	Subordinate mineral (1-10%)
Ore mineral	Malachite	Accessory mineral (<1%)
Ore mineral	Chromite	Accessory mineral (<1%)
Ore mineral	Covellite	Accessory mineral (<1%)
Ore mineral	Digenite	Accessory mineral (<1%)
Ore mineral	Ilmenite	Accessory mineral (<1%)

Relationship	Rock	Origin
Host rock	Conglomerate	Sedimentary Original rock :Conglomerate
		Metamorphic facies :Greenschist
Host rock	Sandstone	Sedimentary Original rock :Sandstone
		Metamorphic facies :Greenschist

Activity:	Test mining	Reserves:
Prod. method:	Underground mining	Production:
Prod. status:	Disused, closed	Volume of dump:

	Location:	Type:	Orientation(360 gr.):	Relation to min.:
	Host rock	Primary layering	Strike/Dip :63 / 55	Pre-mineralisation ;...Effect :Controls

Sample No.	Sample Type	Cu*	Zn*	Pb*	Co*	Ni*	Ag*	Au#
HO-1-1	Bedrock	16970	17	6	1	9	3.8	3.0
HO-1-100	Bedrock	47903	1	3	4	8	6.4	19.0
HO-1-101	Bedrock	16746	1	6	4	9	1.8	14.0
HO-1-102	Bedrock	36772	1	6	13	35	3.7	6.0
HO-1-103	Bedrock	29779	1	2	15	63	4.9	9.0
HO-1-104	Bedrock	47981	1	5	7	22	7.4	13.0
HO-1-2	Bedrock	5931	65	3	3	14	.7	4.0
HO-1-3	Bedrock	3203	12	3	1	21	.1	10.0
HO-1-4	Bedrock	4515	12	3	1	27	.2	3.0
HO-1-5	Bedrock	12441	3	2	7	32	2.6	9.0
HO-1-6	Bedrock	12702	1	5	1	14	5.0	10.0
HO-2-10	Bedrock	22477	1	2	8	30	4.3	12.0
HO-2-105	Bedrock	94	5	3	6	29	.1	1.0
HO-2-106	Bedrock	10740	1	2	7	34	1.8	16.0
HO-2-107	Bedrock	5149	5	3	7	38	.6	3.0
HO-2-108	Bedrock	262	8	2	6	29	.1	1.0
HO-2-109	Bedrock	611	53	6	25	145	.2	1.0
HO-2-11	Bedrock	32413	1	4	7	26	4.8	36.0
HO-2-12	Bedrock	10525	4	2	7	32	.5	34.0
HO-2-7	Bedrock	5757	12	2	8	44	1.1	4.0
HO-2-8	Bedrock	5082	9	2	7	39	1.2	2.0
HO-2-9	Bedrock	7799	9	2	8	42	1.7	3.0
HO-3-110	Bedrock	3047	4	6	8	41	.5	9.0
HO-3-111	Bedrock	1238	3	2	4	28	1.1	3.0
HO-3-112	Bedrock	35954	1	7	10	27	17.9	83.0

Sample No.	Pt#	Pd#	Rh#	As*	Cd*	Ba*	Mo*	Sb*	Bi*
HO-1-1	1.0	2.0	2.0	2	1.0	80	3.00	3	7
HO-1-100	2.0	2.0	2.0	2	1.0	48	32.00	2	2
HO-1-101	2.0	2.0	2.0	2	1.0	22	60.00	2	2
HO-1-102	1.0	2.0	2.0	2	1.0	53	3.00	2	2
HO-1-103	2.0	2.0	2.0	3	1.0	57	10.00	2	2
HO-1-104	2.0	2.0	2.0	2	1.0	56	6.00	2	2
HO-1-2	1.0	2.0	2.0	3	1.0	53	5.00	2	2
HO-1-3	1.0	2.0	2.0	4	1.0	148	2.00	2	2
HO-1-4	2.0	2.0	2.0	3	1.0	90	2.00	2	2
HO-1-5	2.0	2.0	2.0	2	1.0	102	6.00	2	2
HO-1-6	1.0	2.0	2.0	2	1.0	134	9.00	2	8
HO-2-10	4.0	2.0	2.0	2	1.0	169	1.00	2	8
HO-2-105	2.0	2.0	2.0	2	1.0	36	2.00	2	2
HO-2-106	1.0	2.0	2.0	2	1.0	72	2.00	2	2
HO-2-107	2.0	2.0	2.0	2	1.0	87	2.00	2	2
HO-2-108	3.0	3.0	2.0	2	1.0	144	1.00	2	2
HO-2-109	2.0	5.0	2.0	3	1.0	79	2.00	2	4
HO-2-11	3.0	2.0	2.0	3	1.0	38	2.00	2	5
HO-2-12	4.0	2.0	2.0	5	1.0	132	1.00	4	2
HO-2-7	4.0	5.0	2.0	5	1.0	92	1.00	3	2
HO-2-8	1.0	2.0	2.0	2	1.0	110	2.00	2	8
HO-2-9	3.0	3.0	2.0	2	1.0	90	2.00	2	2
HO-3-110	1.0	2.0	2.0	2	1.0	427	2.00	2	2
HO-3-111	1.0	2.0	2.0	2	1.0	47	3.00	2	2
HO-3-112	2.0	2.0	2.0	2	1.0	75	3.00	2	19

Sample No.	S%	V*	Cr*	Mn*	Fe%	Th*	U*	W*	Sr*
HO-1-1	.32	4	18	15	.50	4.00	5.00	1	5.0
HO-1-100	.99	3	14	16	.60	3.00	5.00	1	5.0
HO-1-101	.49	1	21	29	.79	2.00	5.00	1	4.0
HO-1-102	.67	11	100	91	1.61	6.00	5.00	1	3.0
HO-1-103	.66	23	116	120	3.11	9.00	5.00	1	9.0
HO-1-104	.96	8	29	36	1.35	4.00	5.00	1	3.0
HO-1-2	.54	5	35	28	1.26	7.00	5.00	1	4.0
HO-1-3	.28	11	29	38	1.23	5.00	5.00	1	2.0
HO-1-4	.29	8	43	65	1.66	4.00	5.00	1	5.0
HO-1-5	.29	9	39	68	1.24	3.00	5.00	1	4.0
HO-1-6	.15	6	15	23	.62	5.00	5.00	1	5.0
HO-2-10	.44	23	151	66	2.28	7.00	5.00	1	6.0
HO-2-105	.01	8	53	55	1.45	3.00	5.00	1	4.0
HO-2-106	.23	10	63	83	1.53	5.00	5.00	1	3.0
HO-2-107	.13	9	63	80	1.41	5.00	5.00	1	3.0
HO-2-108	.01	8	20	56	.87	7.00	5.00	1	4.0
HO-2-109	.01	46	400	445	3.94	4.00	5.00	1	4.0
HO-2-11	.99	12	87	77	1.60	5.00	5.00	1	9.0
HO-2-12	.89	15	100	93	2.27	4.00	5.00	1	5.0
HO-2-7	.12	13	111	91	1.81	11.00	5.00	1	6.0
HO-2-8	.12	12	93	83	1.86	5.00	5.00	1	6.0
HO-2-9	.22	15	124	91	1.96	16.00	5.00	1	5.0
HO-3-110	.14	14	56	61	2.78	3.00	5.00	1	5.0
HO-3-111	.03	6	36	51	.96	2.00	5.00	1	3.0
HO-3-112	.95	8	100	45	2.12	9.00	5.00	1	2.0