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THE ORE DATABASE | |||||
Deposit Area 1841 - 020 | |||||
(Last updated 15.mai.2006) |
Name of Deposit Area : Kobbertoppen |
(Object Id : 1841,020,00,00) |
The deposit area belongs to the Province : Sulitjelma provins |
Location |
County : | Nordland (18) | Municipality : | Fauske (1841) |
Map 1:50000: | Sulitjelma (2129-2) | Map 1:250000: | Sulitjelma |
Marking point: | Longitude: | 16.0987770 | Latitude: | 67.1560780 |
EU89-UTM Zone 33 | (Coordinates IS confirmed) |
X-coord: | 547599 m. | Y-coord: | 7449200 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Sulphides | |
Element(s): | Kis |
Production |
Activity: | Pitting | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: |
Importance |
Public: | Little Importance (reg. 18.02.2015) |
Economical: | Minor interest |
Products |
Element/product | Crude ore grade or quality | |
CU | 0.1 % |
Operations |
From - To | Activity | Comments | |
1900 - 1900 | Sampling | Company/Institution :Sulitjelma Gruber |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Dating: | Method: | |||
Genesis: | Sedex | Form: | Layer | |
Main texture: | Cataclastic | Min. distribution: | Semi-massive (20-50 % ore minerals) |
Main grain size: | Very unevenly grained | Main alteration: |
Strike/Dip: | 270 / 45 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Ordovician |
Province: | Caledonides | |
Geotec.unit: | Gasak Nappe Complex | |
Tectonic complex: | Kølidekkekomplekset | |
Igneous complex: |
Group: | Småsorjusgruppen | Formation: | Lapphellarformasjonen |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Rustskifer | Sedimentary Original rock :Sandstone |
|
Metamorphic facies :Amphibolite |
Information(s) in free text format |
Free text |
Mineraliseringen på kobbertoppen består av ei mindre linse av magnetkis som ligger som et lag i rusten glimmerskifer, "Lapphellerenskifer". Det er ikke funnet analyser fra mineraliseringen eller analyser fra kjerneboring, slik at kobbergehalten er vurdert visuelt til ca. 0.1 %. Ingen litteratur er funnet. Stien, R. 1993. Tipp på ca. 10 m3 er delvis skjult av ei snøfonn. Rusten kalkstein. Sannsynligvis ligger også skjerpet under snøen. L. F. -94. |
Photo(s) from the Deposit area: |
|
Bibliography: |
From NGU's Reference Archive: |
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 |
Kollung, S. , 1986 |
Sulitjelma. Berggrunnskart; Sulitjelma; 21292; 1:50 000; trykt i farger; |
;Norges geologiske undersøkelse;KART |
Abstract: | |
Opptrykk 1989 |
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. |
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. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
NO0507.02 | Dump |
|
NB! All analyse values are shown at the end of the printout.: |
Name of Locality : Skjerp 1 |
(Object Id : 1841,020,01,00) |
Location |
County : | Nordland (18) | Municipality : | Fauske (1841) |
Map 1:50000: | Sulitjelma (2129-2) | Map 1:250000: | Sulitjelma |
Marking point: | Longitude: | 16.0919350 | Latitude: | 67.1579190 |
EU89-UTM Zone 33 | (Coordinates IS confirmed) |
X-coord: | 547300 m. | Y-coord: | 7449400 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Sulphides | |
Element(s): | Kis |
Production |
Activity: | Pitting | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: |
Information(s) in free text format |
Free text |
Sprengt litt i en rustsone i kvarts/serisittskifer opp for vatna. Ikke synlig kis. L.F. -94 |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
NO0507.01 | Dump |
|
NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 1841 - 020 Kobbertoppen |
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# |
NO0507.01 | Dump | 125 | 53 | 6 | 7 | 26 | -.3 | 2.0 |
NO0507.02 | Dump | 222 | 28 | 7 | 4 | 18 | .6 | 2.0 |
------------------ |
Sample No. | Pt# | Pd# | Rh# | As* | Cd* | Ba* | Mo* | Sb* | Bi* |
NO0507.01 | -3.0 | -3.0 | -5.0 | 55 | -.2 | 300 | 9.00 | -2 | -2 |
NO0507.02 | -3.0 | 3.0 | -5.0 | 13 | -.2 | 23 | 8.00 | -2 | -2 |
------------------ |
Sample No. | S% | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* |
NO0507.01 | .58 | 26 | 32 | 169 | 2.54 | 9.00 | -5.00 | -2 | 44.0 |
NO0507.02 | .32 | 9 | 15 | 174 | 5.03 | 4.00 | -5.00 | -2 | 32.0 |
------------------ |
Sample No. | La* | B* | |||||||
NO0507.01 | 18.00 | 3 | |||||||
NO0507.02 | 5.00 | 4 |
The fact sheet was created on 22.11.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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