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THE ORE DATABASE
Occurence 1833 - 109 Kvannlia
(Object Id: 2876)
(Last updated: 07.03.2017)
Belongs to the Province: Mofjellet sink-bly
Drill Cores: Kvannlia

Location
County: Nordland Municipality: Rana (1833)
Map 1:50000: Storforshei (2027-4) Map 1:250000: Mo i Rana
Coordinate system: EU89-UTM Zone 33
East: 476676 m. North: 7350967 m.
Longitude: 14.4804420 Latitude: 66.2777570
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Resource
Resource Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Resource Subtype: Zinc
Element(s): Zn Cu Pb Au Ag
Importance
Raw material meaning: Not Assessed (reg. 18.02.2015)

Resources and production
Activity: Pitting Reserves:
Operating method: Historical production: ,01 thousand tons


Operations
From - To Activity Comments
1976 - 1976 Geophysics Company/Institution :NGU
1977 - 1977 Geophysics Company/Institution :A/S Sydvaranger
1977 - 1978 Core drilling Company/Institution : "
1979 - 1979 Geophysics Company/Institution :NGU
1980 - 1980 Core drilling Company/Institution :A/S Sydvaranger
1991 - 1991 Geology Company/Institution :NGU - Malmreg.
1992 - 1992 Sampling Company/Institution :Bleikvassli Gruber
1993 - 1993 Core drilling Company/Institution :Bleikvassli Gruber
2007 - 2007 Geophysics Company/Institution :GEXCO Norge AS
TEM, magnetometry
2008 - 2009 Geology Company/Institution :NGU mineralressurser
Mapping and sampling

Mineralization
Era: Proterozoic Period: Neoproterozoic
Genesis: Volcex Form: Ruler
Main texture: Banded Min. distribution: Semi-massive (20-50 % ore minerals)
Main grain size: Medium grained (1-3 mm) Main alteration:
Strike/Dip: 250 / 45 Direction:
Plunge:
Stratigraphic classification of host rock
Era: Proterozoic Period: Neoproterozoic
Province: Caledonides
Geotec.unit: Rødingsfjell Nappe Complex
Tectonic complex: Slagfjelldekket
Igneous complex:
Group: Mofjell Group Formation:

Mineralogy
Relationship Mineral Amount
Gangue mineral Quartz Major mineral (>10%)
Gangue mineral Muscovite Subordinate mineral (1-10%)
Gangue mineral Plagioclase Subordinate mineral (1-10%)
Gangue mineral Potassic feldspar Subordinate mineral (1-10%)
Ore mineral Pyrite Major mineral (>10%)
Ore mineral Sphalerite Subordinate mineral (1-10%)
Ore mineral Pyrrhotite Subordinate mineral (1-10%)
Ore mineral Fahlore Accessory mineral (<1%)
Ore mineral Chalcopyrite Accessory mineral (<1%)
Ore mineral Galena Accessory mineral (<1%)
Ore mineral Arsenopyrite Accessory mineral (<1%)

Lithology:
Relationship Rock Origin
Host rock Muskovittgneis Sedimentary
Original rock :Tuffite
Metamorphic facies :Amphibolite
Wall rock Muskovitt-biotittgn. Sedimentary
Original rock :Mudstone
Metamorphic facies :Amphibolite

Structures
Location: Type: Orientation(360 gr.): Relation to min.:
Host rock Primary layering Strike/Dip :250 / 45 Syn-mineralisation ;...Effect :Controls
Host rock Foliation Strike/Dip :250 / 45 Post-mineralisation ;...Effect :Modifies

Information(s) in free text format
Free text
According to TURAM measurements in 1979 the mineralization at Kvannlia has an extent of 1600 m along strike from the main prospect and eastwards to showing no.1. Two drill holes close to the main prospect to a depth of 200 m only intersected weak impregnations of iron sulfides. The mineralization in the main prospect is c. 3 m thick and consists of bands and lenses of pyrite enrichments in quartz-sericite schist. The most massive lenses are 5-10 cm thick and contain lesser amounts of sphalerite. Some veins and lenses of pyrite with very minor sphalerite, chalcopyrite and galena are present in a c. 30 cm thick quartz rich layer in the footwall of the mineralization. An average of five dump samples collected in 2008 yielded 2.0 % Zn, 0.1 % Cu, <0.1 % Pb and 5 g/t Ag.

Bibliography:
From NGU's Reference Archive:
Bjerkgård, Terje ; Marker, Mogens ; Slagstad, Trond ; Solli, Arne , 2008
Mofjell-prosjektet. Statusrapport 2008
;Norges geologiske undersøkelse;RAPPORT;NGU-rapport; No.2008.088;25 s. pages
Abstract:
Rapporten gir en status for Mofjellprosjektet, et 4-årig samarbeidsprosjekt mellom GEXCO Norge AS og NGU. Prosjektområdet er øst og sør for Mo i Rana, et område som kan inneholde økonomiske sulfidforekomster med Cu, Zn, Pb, Ag og Au. Målet er å få fram dette potensialet gjennom å kartlegge berggrunnen, de kjente og delvis drevne sulfidforekomstene og andre mineraliseringer i området. Berggrunnskartleggingen i 2008 har fokusert på den østlige delen av området, som omfatter fortsettelsen av Plurdalgruppen sørover og relasjonen til bergartsgrupper i øst. Dette innbefatter den viktige tidlig Kaledonske skyvestrukturen som kalles Langfjellsonen, som kan representere et malmgeologisk provinsielt skille, med jernmalmene i nord og sulfidforekomstene i sør. Under feltarbeidet ble det systematisk innsamlet 95 bergartsprøver til geokjemi, geokronologi og petrologi for å undersøke bergartenes dannelse som bakgrunn for relasjonen til malmgenese. Malmgeologiarbeidet har i 2008 fokusert på å skaffe oversikt over sulfidforekomster i Mofjellgruppen og en rekke nøkkelforekomster i de forskjellige mineraliserte sonene er kartlagt og prøvetatt. I tillegg har GEXCO innsamlet mange prøver, dels i form av håndstykkeprøver og dels i form av boring med packsack utstyr. Sammen med resultater fra GEXCOs diamantboringer viser arbeidet så langt at en rekke forekomster og soner i området kan være av økonomisk interesse og bør følges opp videre. De mest interessante områdene og forekomstene i Mofjellgruppen som peker seg ut så langt i tillegg til forekomstene i Mofjellet og Sølvberget er Hellerfjellet, Hesjelia-Hammertjønna, Heramb-Bertelberget og Småvatnan. Mer arbeid med dataene, blant annet sammenholdt med data fra tidligere prospekteringsaktivitet i området, er nødvendig for å komme nærmere inn på potensialet i både de ovenfor nevnte forekomstene og andre i området.

Bjerkgård, Terje; Marker, Mogens; Slagstad, Trond; Solli, Arne , 2013
The Mofjell project: summary and conclusions
;Norges geologiske undersøkelse;RAPPORT;NGU-rapport; No.2013.048;87 pages
Abstract:
The Mofjell project commenced in 2008 as a cooperation between GEXCO Norge AS, the county administration of Nordland and NGU. As GEXCO faced financial difficulties the external funding ended in 2009. The project area included Mofjellet and the eastern part of Plurdalen, an area with a large potential for economic sulfide deposits with Zn, Cu, Pb, Ag and Au. NGU has focused on establishing the geological setting of the Mofjell Group and its relation to ore formation. Another very important goal has been to assess the potential for economic ore deposits in the area, including enrichment of precious metals. On the basis of lithological observations and geochemistry, the Mofjell Group consists of a largely bimodal volcanic-sedimentary assemblage formed in an island-arc to back-arc setting. The data also show that the proportion of felsic volcanic rocks is much higher than previously described. A bimodal volcanic suite mixed with sediments is a geological environment which is regarded as favorable for both rich and large sulfide deposits.

Singsaas, Per , 1980
Turammålinger Raudvatnet,Rana
;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.1760;10 pages
Abstract:
Turam-oppdraget gikk ut på å måle et område av ca. 2 km lengde, og den primære oppgaven var å klarlegge spørsmål vedrørende eventuelle dypereliggende ledere. Det er skjerpet flere steder i feltet. I det viktigste skjerpet sees svovel- kis og magnetkis med kobberkis, sinkblende og blyglans, ca. 2 meter kompaktkis og 1.5 meter impregnasjon. Ved målingene ble det påvist flere ledende soner av betydlig feltutstrekning. Sonene har varierende ledningsevne og ligger i noe forskjellige dyp. Det vil være aktuelt å utføre sonderende diamantboringer på et par soner.

Søvegjarto, U.; Marker, M.; Gjelle, S. , 1989
Storforshei. Berggrunnskart; Storforshei; 20274; 1:50 000; trykt i farger;
;Norges geologiske undersøkelse;KART

References not to be found in NGU's Reference Archive.:
Marker, M. 1980: Geologien i et område umiddelbart vest for Raudvatnet. Upubl.- rapp.


Endresen, B.A. 1972: Sulfidlokaliteter i Rana - kort oversikt med forsøk på kvalitativ kartlegging. Upubl. rapp.


Kruse, A. 1981: Diamantboring Raudvatn, Rana, Nordland 1980. Intern rapport nr. 8104, Bergverksselskapet Nord-Norge A/S.

Fieldsamples
Sample No. Sample type Miscellanrous
KV-01 Bedrock
Sampler: T. Bjerkgård/...Stored: Løkken
Comment: Quartz-sericite schist with impregnation of py and minor sl, accessory cpy and ga
No. of registrated element analyses = 1
KV-02 Bedrock
Sampler: T. Bjerkgård/...Stored: Løkken
Comment: Semimassive py with some sl
No. of registrated element analyses = 1
NO0772.05 Bedrock
Sampler: Wilberg, R./...Stored: Løkken
Comment: Lys muskovittskifer med py-diss.
No. of registrated element analyses = 1
NO0772.06 Bedrock
Sampler: Wilberg, R./...Stored: Løkken
Comment: Muskovittskifer med py-po-sl-diss.
No. of registrated element analyses = 1
NO0772.07 Bedrock
Sampler: Wilberg, R./...Stored: Løkken
Comment: Glimmerskifer med cpy-py-diss.
No. of registrated element analyses = 1
NO0772.08 Bedrock
Sampler: Wilberg, R./...Stored: Løkken
Comment: Massiv py-sl-po-malm.
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:

Name of Locality: Skjerp 1
(Object Id: 3702 109,01,00)

Location
County: Nordland Municipality: Rana (1833)
Map 1:50000: Storforshei (2027-4) Map 1:250000: Mo i Rana
Coordinate system: EU89-UTM Zone 33
East: 475692 m. North: 7350775 m.
Longitude: 14.4585610 Latitude: 66.2759600
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 Au Ag
Resources and production
Activity: Pitting Reserves:
Operating method: Historical production:


Information(s) in free text format
Free text
Showing no. 1 consists of thin bands and lenses of sulfides associated with quartz seg-regations in sericite schist. The sulfides include pyrite, sphalerite, galena and arsenopyrite and the whole zone is 20-40 cm thick. This showing shows very high gold contents (up to 27 g/t and an average of 7 samples is 7 g/t) and also silver (up to 283 g/t and average 89 g/t), which correlate well with enrichments of arsenic (up to 0.3 %). The nature of the mineralization shows that this is a secondary enrichment, probably due to the strong deformation and intense folding in the area.

Fieldsamples
Sample No. Sample type Miscellanrous
KV-04 Bedrock
Sampler: T. Bjerkgård/...Stored: Løkken
Comment: Weak py impregnation in quartz-sericite schist
No. of registrated element analyses = 1
NO0772.02 Bedrock
Sampler: Wilberg, R./...Stored: Løkken
Comment: Muskovittskifer med py-ga-sl-disseminasjon.
No. of registrated element analyses = 1
NO0772.03 Bedrock
Sampler: Wilberg, R./...Stored: Løkken
Comment: Muskovittskifer med py-po-sl-diss.
No. of registrated element analyses = 1
NO0772.04 Bedrock
Sampler: Wilberg, R./...Stored: Løkken
Comment: Muskovittskifer med py-ga-sl-disseminasjon.
No. of registrated element analyses = 1
NO0772.09 Bedrock
Sampler: Wilberg, R./...Stored: Løkken
Comment: Musk.gneis med sulfid-diss.
No. of registrated element analyses = 1
NO0772.10 Bedrock
Sampler: Wilberg, R./...Stored: Løkken
Comment: Musk.gneis med sulfid-diss.
No. of registrated element analyses = 1
NO0772.11 Bedrock
Sampler: Wilberg, R./...Stored: Løkken
Comment: Musk.gneis med sulfid-diss.
No. of registrated element analyses = 1
NO0772.12 Bedrock
Sampler: Wilberg, R./...Stored: Løkken
Comment: Musk.gneis med sulfid-diss.
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:

Name of Locality: Skjerp 2
(Object Id: 3703 109,02,00)

Location
County: Nordland Municipality: Rana (1833)
Map 1:50000: Storforshei (2027-4) Map 1:250000: Mo i Rana
Coordinate system: EU89-UTM Zone 33
East: 475671 m. North: 7350783 m.
Longitude: 14.4580920 Latitude: 66.2760300
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 Au Ag
Resources and production
Activity: Pitting Reserves:
Operating method: Historical production:


Information(s) in free text format
Free text
20 m mot VNV: Skjerp 2 (< 1 m3 tipp) i hengberget til ovennevnte. Over knapt 50 cm mektighet er svovelkis, sinkblende, og blyglans disseminert i lys, rusten muskovittgneis (5-8 % sulfider). Granat-glimmergneis i heng.

Fieldsamples
Sample No. Sample type Miscellanrous
KV-03 Bedrock
Sampler: T. Bjerkgård/...Stored: Løkken
Comment: Very weak py impregnation in muscovite-biotite gneiss
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:

Name of Locality: Skjerp 3
(Object Id: 3704 109,03,00)

Location
County: Nordland Municipality: Rana (1833)
Map 1:50000: Storforshei (2027-4) Map 1:250000: Mo i Rana
Coordinate system: EU89-UTM Zone 33
East: 475815 m. North: 7351278 m.
Longitude: 14.4612260 Latitude: 66.2804820
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 Au Ag
Resources and production
Activity: Pitting Reserves:
Operating method: Historical production:


Information(s) in free text format
Free text
I skjerp 3 er det sprengt ut < 1 m3 i en lys, rusten, finkornet muskovittgneis med svovelkis- og magnetkis-disseminasjon (5 %, 01).

Fieldsamples
Sample No. Sample type Miscellanrous
KV-05 Bedrock
Sampler: T. Bjerkgård/...Stored: Løkken
Comment: Quartz-veins with relatively rich py impregnation, some po, possibly sl and cpy
No. of registrated element analyses = 1
NO0772.01 Bedrock
Sampler: Wilberg, R./...Stored: Løkken
Comment: Lys, finkornet muskovittgneis med py- og po-diss.
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:


Analyse Results
from
Deposit Area 1833 - 109 Kvannlia

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#
KV-01 Bedrock 535 23600 72 15 6 1.0 10.0
KV-02 Bedrock 1130 7500 43 26 7 2.0 70.0
KV-03 Bedrock 305 3190 684 7 -5 7.0 90.0
KV-04 Bedrock 333 1880 811 8 -5 5.0 240.0
KV-05 Bedrock 56 118 211 9 21 1.0 10.0
NO0772.01 Bedrock 22 125 7 6 23 .4 4.0
NO0772.02 Bedrock 1030 7180 21749 10 5 283.9 27669.0
NO0772.03 Bedrock 1000 1917 21783 9 8 249.1 15656.0
NO0772.04 Bedrock 898 8726 1545 7 6 12.7 187.0
NO0772.05 Bedrock 38 259 213 11 7 5.7 191.0
NO0772.06 Bedrock 1266 32521 201 13 36 7.4 96.0
NO0772.07 Bedrock 1848 2740 351 8 7 9.8 82.0
NO0772.08 Bedrock 534 32132 139 32 17 6.0 79.0
NO0772.09 Bedrock 276 2504 1243 6 4 28.9 1772.0
NO0772.10 Bedrock 199 1885 2112 6 4 18.1 191.0
NO0772.11 Bedrock 195 1798 1863 6 4 16.0 307.0
NO0772.12 Bedrock 142 1122 632 5 3 16.5 2590.0
------------------
Sample No. Pt# Pd# As* Cd* Ba* Mo* Sn* Sb* Bi*
KV-01 664 14.00 21
KV-02 454 23.00 14
KV-03 684 6.00 5
KV-04 521 3.00 25
KV-05 173 17.00 1
NO0772.01 7.0 4.0 31 .5 22 7.00 2 2
NO0772.02 8.0 2.0 2653 43.8 15 6.00 510 27
NO0772.03 18.0 1.0 2781 22.3 16 5.00 491 38
NO0772.04 14.0 1.0 57 66.4 29 8.00 9 6
NO0772.05 19.0 5.0 269 .2 3 11.00 6 3
NO0772.06 16.0 6.0 145 208.0 6 12.00 20 15
NO0772.07 14.0 1.0 73 14.0 24 4.00 13 2
NO0772.08 10.0 1.0 276 183.7 3 7.00 20 7
NO0772.09 3.0 3.0 256 14.9 26 5.00 29 2
NO0772.10 3.0 3.0 140 12.1 26 3.00 17 9
NO0772.11 3.0 3.0 125 11.0 25 3.00 13 5
NO0772.12 3.0 3.0 253 6.5 32 2.00 22 2
------------------
Sample No. Ga* S% V* Cr* Mn* Fe% Th* U* W*
KV-01 14.00 43 20 232 17.26 1.00 3.00 5
KV-02 7.00 21 10 155 27.14 2.00 2.00 6
KV-03 15.00 59 10 387 4.80 3.00 2.00 5
KV-04 18.00 49 10 232 3.85 2.00 1.00 2
KV-05 13.00 119 10 775 11.74 3.00 6.00 4
NO0772.01 2.97 20 7 132 4.56 1.00 5.00 1
NO0772.02 8.77 3 4 124 7.81 5.00 5.00 13
NO0772.03 6.09 3 9 86 5.74 5.00 5.00 2
NO0772.04 4.19 1 4 71 4.15 6.00 5.00 4
NO0772.05 10.08 1 2 76 9.53 1.00 5.00 1
NO0772.06 22.13 1 5 450 28.36 6.00 9.00 1
NO0772.07 2.99 43 13 272 3.67 1.00 5.00 2
NO0772.08 26.90 2 1 426 26.40 5.00 5.00 1
NO0772.09 6.22 8 2 90 4.94 2.00 5.00 1
NO0772.10 4.49 4 3 51 4.59 3.00 7.00 1
NO0772.11 4.24 4 4 50 4.61 3.00 5.00 1
NO0772.12 3.80 2 2 31 3.63 3.00 9.00 1
------------------
Sample No. Rb* Sr* Y* Zr* Nb* Ta* La* Ce* B*
KV-01 28.0 26.0 4.0 36 3.00 -1.00 4.00 5.00
KV-02 20.0 16.0 2.0 26 2.00 -1.00 4.00 3.00
KV-03 47.0 72.0 11.0 67 2.00 -1.00 5.00 6.00
KV-04 39.0 57.0 8.0 71 2.00 -1.00 -1.00 -1.00
KV-05 31.0 133.0 34.0 57 3.00 -1.00 12.00 29.00
NO0772.01 1.0 4.00 2
NO0772.02 2.0 4.00 3
NO0772.03 2.0 3.00 2
NO0772.04 1.0 2.00 2
NO0772.05 1.0 2.00 2
NO0772.06 1.0 2.00 35
NO0772.07 4.0 2.00 2
NO0772.08 1.0 2.00 35
NO0772.09 2.0 2.00 2
NO0772.10 2.0 2.00 3
NO0772.11 2.0 2.00 3
NO0772.12 2.0 2.00 2
------------------
Sample No. Hf*
KV-01 1.00
KV-02
KV-03
KV-04
KV-05 2.00
NO0772.01
NO0772.02
NO0772.03
NO0772.04
NO0772.05
NO0772.06
NO0772.07
NO0772.08
NO0772.09
NO0772.10
NO0772.11
NO0772.12


The fact sheet was created on 29.04.2024

Questions or comments regarding the fact sheet can be emailed to:
ressursdatabaser@ngu.no
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