English version
MALMDATABASEN
Forekomstområde 1841 - 018
(Sist oppdatert 11.okt.2018)

Navn på deposit area : Mons Petter
(Objekt Id : 1841,018,00,00)
Forekomstområdet tilhører provinsen : Sulitjelma provins

Lokalisering
Fylke : Nordland (18) Kommune : Fauske (1841)
Kart 1:50000: Sulitjelma (2129-2) Kart 1:250000: Sulitjelma
Markeringspunkt: Lengdegrad: 16.0343530 Breddegrad: 67.1430200
EU89-UTM Zone 33 (Coordinates IS confirmed)
X-koord: 544833 m. Y-koord: 7447696 m.

Materialtype
Hovedtype: Basemetaller (Cu,Zn,Pb,Fe sulfider,As,Sb,Bi,Sn) Subtype: Kobber
Element(s): Cu Zn Kis Co
Production
Activity: Gruvedrift Reserves:
Prod. method: Underjordsdrift Production: 2500 thousand tons
Prod. status: Nedlagt Volume of dump:

Betydning
Offentlig: Little Importance (reg. 01.06.2015)
Economical: Viktig , (Confirmed 12.feb.2005 by Are Korneliussen)

Products
Element/product Crude ore grade or quality
CU 1.75 %
KIS 20 %
ZN 0.48 %

Operations
From - To Activity Comments
1886 - 1986 Geology Company/Institution : " "
1887 - 1985 Core drilling Company/Institution : " "
1887 - 1986 Regular production Company/Institution :Sulitjelma Gruber A/S
1941 - 1984 Geophysics Company/Institution : " "

Mineralization
Era: Paleozoic Period: Ordovician
Dating: Method:
Genesis: Vulkeks Form: Linse
Main texture: Kataklastisk Min. distribution: Massiv
Main grain size: Meget ujevnkornet Main alteration: Klorittisering
Strike/Dip: 220 / 20 Direction:
Plunge:
Stratigraphic classification of host rock
Era: Paleozoic Period: Ordovician
Province: Caledonides
Geotec.unit: Køli Nappe Complex
Tectonic complex:
Igneous complex:
Group: Sulitjelmagruppen Formation: Otervassformasjonen

Mineralogy
Relationship Mineral Amount
Gangue mineral Chlorite Major mineral (>10%)
Gangue mineral Biotite Major mineral (>10%)
Ore mineral Pyrite Major mineral (>10%)
Ore mineral Sphalerite Major mineral (>10%)
Ore mineral Chalcopyrite Major mineral (>10%)

Lithology:
Relationship Rock Origin
Host rock Klorittbreksje Extrusive
Original rock :Basalt
Metamorphic facies :Amphibolite
Host rock Biotittbreksje Extrusive
Original rock :Basalt
Metamorphic facies :Amphibolite
Wall rock Amfibolitt Extrusive
Original rock :Tuff
Metamorphic facies :Amphibolite

Structures
Location: Type: Orientation(360 gr.): Relation to min.:
Host rock Fold axis Strike/Dip :220 / 20 Post-mineralisation ;...Effect :Controls

Opplysning(er) i fritekstformat
Fri tekst
Mons Petter-forekomsten er delt inn i Mons Petter I og II, og var den første malm som det ble produsert fra i Sulitjelma. Mons Petter II ble påvist i 1971 etter omfattende diamantboring og andre undersøkelser. Rik forekomst, lett produserbar malm med enkel transport og mektigheter opp i 12 m. Malmen er deformert ved en større isoklinalfolding. En rekke borkjerner fra mange borhull ligger på lager i Sulitjelma. Stien, R. 1993. To gamle tipper fra stollinnslag i ca 300 m.o.h. rett ovenfor Sulitjelma Grubers administrasjonsbygg prøvetas. Furuhaug, L. 1994.

Bibliography:
From NGU's Reference Archive:
Boyle, A.P.; Hansen, T.S.; Mason, R.; , 1985
A new tectonic perspective of the Sulitjelma Region. I The Caledonide Orogen - Scandinavia and Related Areas, Red: D.G. Gee & B.A. Sturt
;John Wiley & Sons Ltd;ARTIKKEL;529-542 pages

Sulitjelma gruber. Oversiktskart over feltet
;Norges geologiske undersøkelse;KART;Bergarkivet; No.K 1205

Cook, N. , 1996
Mineralogy of the sulphide deposits at Sulitjelma, northern Norway
;ARTIKKEL;Ore geology reviews; No.11;303-338 pages

Eidsvig, Per , 1973
Måling av oppladet potensial ved Mons Petter og Bursi.
;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.1123;10 pages

Kollung, S. , 1986
Sulitjelma. Berggrunnskart; Sulitjelma; 21292; 1:50 000; trykt i farger;
;Norges geologiske undersøkelse;KART
Abstract:
Opptrykk 1989

Kollung, Sigbjørn , 1989
Sulitjelmafeltet. Berggrunnsgeologisk kart - M 1 : 100 000. Beskrivelse.
;Norges geologiske undersøkelse;BOK; KARTBESKRIVELSE;Skrifter; No.93;1 - 47 pages
Abstract:
The eugeoclinal rocks of the Sulitjelma region occup a large depression in the Norwegian Caldonodrd betwwen the Nasafjell tectonic window of Precambrian rocks in the south and the Tysfjord window in the north. The age of the rocks is thought to be Cambro-Silurian. The regionl metamophism is mainly in greenschist facies in the lower units, amphibolite facies in the Gasak Nappe and greenschist to amphibolite facies in the Fauske Nappe. Some of the largest sulphide deposits in Norway are located near Sulitjelma. The different types of mineralizations occurring in the region are briefly described.

Krog, Jan Reidar; Næss, Gunnar , 1987
Geokjemiske undersøkelser av bekkesedimenter i Sulitjelma-området.
;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.86.047;59 pages
Abstract:
Bekkesedimenter fra 334 prøvelokaliteter i Sulitjelma-området ble innsamlet med en prøvetetthet på 1 prøve pr. 10 km2. Rapporten inneholder tabeller og resultkart over 28 elementer oppsluttet med HNO3 og bestemt med ICAP.

Hansen, Tor Søyland , 1982
En geologisk undersøkelse av Nordgruvefeltet i Sulitjelma
;NTH Bergavd.;AVHANDLING;354 bl. pages
Abstract:
Dr.ing. avh. ved Norges tekniske høgskole, Trondheim, mars 1982

Christoffersen, T.M. , 1960
Malmgeologisk beskrivelse av området Bursi-Charlotta, Sulitjelma.
;NTH Bergavd.;AVHANDLING

Navn på sample point : Prøvepunkt 1
(Objekt Id : 1841,018,00,01)

Lokalisering
Fylke : Nordland (18) Kommune : Fauske (1841)
Kart 1:50000: Sulitjelma (2129-2) Kart 1:250000: Sulitjelma
Markeringspunkt: Lengdegrad: 16.0354680 Breddegrad: 67.1421150
EU89-UTM Zone 33 (Coordinates IS confirmed)
X-koord: 544883 m. Y-koord: 7447596 m.

Materialtype
Hovedtype: Basemetaller (Cu,Zn,Pb,Fe sulfider,As,Sb,Bi,Sn) Subtype: Kobber
Element(s): Cu Zn Kis


Fieldsamples
Sample No. Sample type Miscellanrous
NO0505.01 Dump
Sampler :Furuhaug, L./...Stored :Løkken
Kommentar :Diss. cpy-py. Rel. grovk.
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:

Navn på sample point : Prøvepunkt 2
(Objekt Id : 1841,018,00,02)

Lokalisering
Fylke : Nordland (18) Kommune : Fauske (1841)
Kart 1:50000: Sulitjelma (2129-2) Kart 1:250000: Sulitjelma
Markeringspunkt: Lengdegrad: 16.0366210 Breddegrad: 67.1421080
EU89-UTM Zone 33 (Coordinates IS confirmed)
X-koord: 544933 m. Y-koord: 7447596 m.

Materialtype
Hovedtype: Basemetaller (Cu,Zn,Pb,Fe sulfider,As,Sb,Bi,Sn) Subtype: Kobber
Element(s): Cu Zn Kis


Fieldsamples
Sample No. Sample type Miscellanrous
NO0505.02 Dump
Sampler :Furuhaug, L./...Stored :Løkken
Kommentar :Diss. cpy-py. Rel. grovk.
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:

Navn på sample point : Bh 127A/B/F/G
(Objekt Id : 1841,018,00,03)

Lokalisering
Fylke : Nordland (18) Kommune : Fauske (1841)
Kart 1:50000: Sulitjelma (2129-2) Kart 1:250000: Sulitjelma
Markeringspunkt: Lengdegrad: 16.0413290 Breddegrad: 67.1434800
EU89-UTM Zone 33 (Coordinates IS confirmed)
X-koord: 545135 m. Y-koord: 7447752 m.

Materialtype
Hovedtype: Basemetaller (Cu,Zn,Pb,Fe sulfider,As,Sb,Bi,Sn) Subtype: Kobber
Element(s): Cu Zn Kis Co


Fieldsamples
Sample No. Sample type Miscellanrous
Bh127A,136.45-137.46 Core
Sampler :T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
Bh127B,158.00-159.00 Core
Sampler :T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
Bh127F,163.90-164.70 Core
Sampler :T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
Bh127G,157.00-158.20 Core
Sampler :T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:

Navn på sample point : Bh 23 C2
(Objekt Id : 1841,018,00,04)

Lokalisering
Fylke : Nordland (18) Kommune : Fauske (1841)
Kart 1:50000: Sulitjelma (2129-2) Kart 1:250000: Sulitjelma
Markeringspunkt: Lengdegrad: 16.0459480 Breddegrad: 67.1473170
EU89-UTM Zone 33 (Coordinates IS confirmed)
X-koord: 545328 m. Y-koord: 7448184 m.

Materialtype
Hovedtype: Basemetaller (Cu,Zn,Pb,Fe sulfider,As,Sb,Bi,Sn) Subtype: Kobber
Element(s): Cu Zn Kis Co


Fieldsamples
Sample No. Sample type Miscellanrous
Bh23 C2, 41.15-42.75 Core
Sampler :T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:

Navn på sample point : Bh 1B
(Objekt Id : 1841,018,00,05)

Lokalisering
Fylke : Nordland (18) Kommune : Fauske (1841)
Kart 1:50000: Sulitjelma (2129-2) Kart 1:250000: Sulitjelma
Markeringspunkt: Lengdegrad: 16.0420950 Breddegrad: 67.1436010
EU89-UTM Zone 33 (Coordinates IS confirmed)
X-koord: 545167 m. Y-koord: 7447767 m.

Materialtype
Hovedtype: Basemetaller (Cu,Zn,Pb,Fe sulfider,As,Sb,Bi,Sn) Subtype: Kobber
Element(s): Cu Zn Kis Co


Fieldsamples
Sample No. Sample type Miscellanrous
Bh1B, 71.90-72.90 Core
Sampler :T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
Bh1B, 72.90-73.90 Core
Sampler :T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:

Navn på sample point : Bh 22O/W
(Objekt Id : 1841,018,00,06)

Lokalisering
Fylke : Nordland (18) Kommune : Fauske (1841)
Kart 1:50000: Sulitjelma (2129-2) Kart 1:250000: Sulitjelma
Markeringspunkt: Lengdegrad: 16.0470920 Breddegrad: 67.1465650
EU89-UTM Zone 33 (Coordinates IS confirmed)
X-koord: 545378 m. Y-koord: 7448101 m.

Materialtype
Hovedtype: Basemetaller (Cu,Zn,Pb,Fe sulfider,As,Sb,Bi,Sn) Subtype: Kobber
Element(s): Cu Zn Kis Co


Fieldsamples
Sample No. Sample type Miscellanrous
Bh22O, 59.30-60.30 Core
Sampler :T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
Bh22O, 61.30-62.40 Core
Sampler :T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
Bh22W, 38.00-39.00 Core
Sampler :T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
Bh22W, 45.15-46.00 Core
Sampler :T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:


Analyse Results
from
Forekomstområde 1841 - 018 Mons Petter

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#
Bh1B, 71.90-72.90 Core 42800 10750 57 511 17 11.9 247.0
Bh1B, 72.90-73.90 Core 23300 2760 33 308 16 6.2 70.0
Bh127A,136.45-137.46 Core 18150 11050 94 223 19 5.9 70.0
Bh127B,158.00-159.00 Core 91400 8760 267 344 17 28.5 530.0
Bh127F,163.90-164.70 Core 20800 9460 117 319 19 7.7 84.0
Bh127G,157.00-158.20 Core 92900 7270 95 348 21 24.7 135.0
Bh22O, 59.30-60.30 Core 13050 5020 106 652 20 5.1 29.0
Bh22O, 61.30-62.40 Core 116000 12950 34 478 13 29.6 122.0
Bh22W, 38.00-39.00 Core 48500 4840 26 357 16 12.7 34.0
Bh22W, 45.15-46.00 Core 68200 8400 113 560 18 17.8 167.0
Bh23 C2, 41.15-42.75 Core 51300 5750 44 558 15 12.4 302.0
NO0505.01 Dump 56154 951 -3 204 81 16.2 129.0
NO0505.02 Dump 10005 3224 70 370 35 7.0 133.0
------------------
Sample No. Pt# Pd# Rh# As* Cd* Ba* Mo* Sn* Sb*
Bh1B, 71.90-72.90 2.5 1.0 234 38.6 50 126.00 6 1
Bh1B, 72.90-73.90 2.5 1.0 226 10.3 5 78.90 2 1
Bh127A,136.45-137.46 2.5 .5 65 38.2 10 66.30 4 0
Bh127B,158.00-159.00 2.5 .5 150 37.7 10 99.80 4 1
Bh127F,163.90-164.70 2.5 .5 120 40.3 30 113.00 4 1
Bh127G,157.00-158.20 2.5 .5 132 33.0 5 83.70 5 1
Bh22O, 59.30-60.30 2.5 .5 260 21.5 5 124.00 2 1
Bh22O, 61.30-62.40 2.5 .5 194 56.4 5 79.70 5 0
Bh22W, 38.00-39.00 2.5 1.0 113 23.6 10 133.00 3 1
Bh22W, 45.15-46.00 2.5 .5 125 29.8 5 84.20 5 1
Bh23 C2, 41.15-42.75 2.5 1.0 124 28.5 10 125.00 5 1
NO0505.01 -3.0 -3.0 -5.0 19 8.2 2 68.00 8
NO0505.02 -3.0 -3.0 -5.0 111 10.7 9 18.00 4
------------------
Sample No. Bi* Se* Ga* Ge* In* S% V* Cr* Mn*
Bh1B, 71.90-72.90 6 99.00 5.85 0.54 2.10 10.00 25 13 101
Bh1B, 72.90-73.90 4 72.00 2.26 0.47 1.02 10.00 14 2 29
Bh127A,136.45-137.46 6 86.00 7.63 0.49 1.90 10.00 47 34 246
Bh127B,158.00-159.00 17 115.00 3.52 0.51 1.87 10.00 20 4 100
Bh127F,163.90-164.70 8 75.00 16.45 0.44 1.54 10.00 58 33 269
Bh127G,157.00-158.20 13 98.00 6.36 0.56 2.10 10.00 34 16 111
Bh22O, 59.30-60.30 30 124.00 1.16 0.56 0.60 10.00 9 3 219
Bh22O, 61.30-62.40 10 127.00 5.57 0.66 1.81 10.00 9 4 151
Bh22W, 38.00-39.00 7 95.00 8.03 0.56 1.35 10.00 21 10 227
Bh22W, 45.15-46.00 14 103.00 13.05 0.51 1.53 10.00 46 39 291
Bh23 C2, 41.15-42.75 10 114.00 3.46 0.57 1.22 10.00 17 4 119
NO0505.01 -2 13.58 62 52 566
NO0505.02 -2 21.51 56 59 225
------------------
Sample No. Fe% Th* U* W* Rb* Sr* Y* Zr* Nb*
Bh1B, 71.90-72.90 41.50 0.08 0.70 0 8.8 2.0 2.8 8 0.20
Bh1B, 72.90-73.90 44.20 0.01 1.30 0 0.3 0.5 0.2 1 0.05
Bh127A,136.45-137.46 36.80 0.33 1.20 0 0.9 10.8 8.4 24 1.30
Bh127B,158.00-159.00 39.80 0.05 1.10 0 2.2 4.9 1.0 4 0.10
Bh127F,163.90-164.70 36.10 1.14 1.10 0 9.9 14.1 8.1 60 1.10
Bh127G,157.00-158.20 37.70 0.22 0.80 0 0.5 5.1 3.9 13 0.30
Bh22O, 59.30-60.30 40.80 0.02 0.40 0 0.1 34.5 0.8 1 0.05
Bh22O, 61.30-62.40 38.00 0.09 0.50 0 0.6 9.1 1.3 5 0.10
Bh22W, 38.00-39.00 38.30 0.81 1.50 0 0.5 19.5 10.2 52 1.10
Bh22W, 45.15-46.00 31.60 0.29 0.60 0 0.1 11.2 8.3 26 0.90
Bh23 C2, 41.15-42.75 40.40 0.26 1.00 1 0.9 3.8 2.3 14 0.40
NO0505.01 21.44 2.00 -5.00 -2 7.0
NO0505.02 22.23 -2.00 -5.00 -2 7.0
------------------
Sample No. Ta* Cs* La* Ce* B* Li* Be* P* Sc*
Bh1B, 71.90-72.90 0.03 2.99 0.70 1.64 3 0 20 1.80
Bh1B, 72.90-73.90 0.03 0.46 0.25 0.17 1 0 5 0.20
Bh127A,136.45-137.46 0.10 0.95 2.20 5.81 5 0 200 4.70
Bh127B,158.00-159.00 0.03 1.41 0.25 0.67 1 0 5 0.50
Bh127F,163.90-164.70 0.10 4.25 3.90 9.05 12 0 220 6.40
Bh127G,157.00-158.20 0.03 1.21 1.20 2.79 2 0 60 2.70
Bh22O, 59.30-60.30 0.03 0.23 0.25 0.79 0 0 20 0.30
Bh22O, 61.30-62.40 0.03 1.80 0.80 1.55 0 0 10 0.20
Bh22W, 38.00-39.00 0.10 0.63 4.00 9.62 3 0 60 2.20
Bh22W, 45.15-46.00 0.10 0.33 1.90 4.63 7 0 190 5.70
Bh23 C2, 41.15-42.75 0.03 0.57 1.30 2.81 1 0 5 0.60
NO0505.01 7.00 -3
NO0505.02 2.00 4
------------------
Sample No. Ti* Te* Hf* Re* Tl*
Bh1B, 71.90-72.90 430 3.03 0.20 0 0
Bh1B, 72.90-73.90 25 1.17 0.05 0 0
Bh127A,136.45-137.46 1990 2.05 0.60 0 0
Bh127B,158.00-159.00 100 7.00 0.10 0 0
Bh127F,163.90-164.70 1250 2.42 1.40 0 0
Bh127G,157.00-158.20 510 5.95 0.30 0 0
Bh22O, 59.30-60.30 25 2.05 0.05 0 0
Bh22O, 61.30-62.40 25 5.57 0.10 0 0
Bh22W, 38.00-39.00 690 4.05 1.20 0 0
Bh22W, 45.15-46.00 1510 3.45 0.60 0 0
Bh23 C2, 41.15-42.75 130 4.83 0.30 0 0
NO0505.01
NO0505.02


Faktaarket ble generert 13.06.2026

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