Norsk versjon | |||||
THE ORE DATABASE | |||||
Deposit 5026 - 011 Killingdal | |||||
(Object Id: 4403) (Last updated: 07.11.2023) |
Drill Cores: Killingdal |
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Location |
County: | Trøndelag | Municipality: | Holtålen (5026) |
Map 1:50000: | Ålen (1720-4) | Map 1:250000: | Røros |
Coordinate system: | EU89-UTM Zone 32 |
East: | 626124 m. | North: | 6965217 m. |
Longitude: | 11.4731540 | Latitude: | 62.7954240 |
Show on map |
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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 Kis |
Importance |
Raw material meaning: | Little Importance (reg. 18.02.2015) |
Resources and production |
Activity: | Mining | Reserves: | 283 thousand tons | |
Operating method: | Underground mining | Historical production: | 2959 thousand tons |
Products |
Element/product | Crude ore grade or quality | Reg. date | |
Cu | 1,7 % | 24.09.2001 | |
Pb | 0,4 % | 24.09.2001 | |
S | 45,0 % | 24.09.2001 | |
Zn | 5,5 % | 24.09.2001 |
Operations |
From - To | Activity | Comments | |
1677 - 1692 | Regular production | Company/Institution :Røros Kobberverk o.a. | |
Nordre grube | |||
1791 - 1809 | Regular production | Company/Institution :Røros Kobberverk | |
Søndre grube | |||
1822 - 1890 | Test mining | Company/Institution :Diverse interessenter | |
1891 - 1986 | Regular production | Company/Institution :A/S Killingdal Grubeselskap | |
Ulike eiere: 1888-1895 A. Huitfeldt & Co. 1895-1945 leid av The Bede Metal & Chemical Co. Ltd. |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Genesis: | Volcex | Form: | Plate | |
Main texture: | Banded | Min. distribution: | Massive (>50 % ore minerals) |
Main grain size: | Fine grained (< 1 mm) | Main alteration: | Sericitisation |
Strike/Dip: | Direction: | 270 | ||
Plunge: | 30 |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Ordovician |
Province: | Caledonides | |
Geotec.unit: | Trondheim Nappe Complex | |
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: | Hersjø |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Calcite | Subordinate mineral (1-10%) | |
Gangue mineral | Chlorite | Subordinate mineral (1-10%) | |
Gangue mineral | Muscovite | Subordinate mineral (1-10%) | |
Ore mineral | Sphalerite | Major mineral (>10%) | |
Ore mineral | Pyrite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Subordinate mineral (1-10%) | |
Ore mineral | Chalcopyrite | Subordinate mineral (1-10%) | |
Ore mineral | Bournonite | Accessory mineral (<1%) | |
Ore mineral | Molybdenite | Accessory mineral (<1%) | |
Ore mineral | Mackinawite | Accessory mineral (<1%) | |
Ore mineral | Tetrahedrite | Accessory mineral (<1%) | |
Ore mineral | Arsenopyrite | Accessory mineral (<1%) | |
Ore mineral | Galena | Accessory mineral (<1%) | |
Ore mineral | Covellite | Accessory mineral (<1%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Hornblende schist | Extrusive Original rock :Basalt |
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Metamorphic facies :Greenschist | |||
Wall rock | Quartz-sericite schist | Extrusive Original rock :Basalt |
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Metamorphic facies :Greenschist | |||
Wall rock | Chlorite schist | Extrusive Original rock :Basalt |
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Metamorphic facies :Greenschist | |||
Wall rock | Calcareous phyllite | Sedimentary Original rock :Argillaceous sediment |
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Metamorphic facies :Greenschist |
Information(s) in free text format |
Free text |
The Killingdal deposit is hosted by massive greenstone, locally with relict pillow structures. There also are subordinate thin layers of felsic metavolcanic rocks in the area. The deposit consists of two ore bodies, the Main Orebody and the North Orebody, which are strongly elongated, with approximately lens-shaped cross sections and occur in the hinge of a regional-scale, isoclinal fold structure. The ore bodies are parallel for about 2500 m of known length and dips about 30o W. At higher levels, the width of the Main Orebody varies at 40–80 m, and has a mean thickness of about 3.5 m, with a maximum at 10–12 m. The cross section of the North Orebody is considerably less than that of the Main Orebody and it has been exploited to a lesser extent. Pyrite is the dominant mineral, while sphalerite and chalcopyrite are subordinate phases. The principal gangue minerals are quartz and muscovite. Bands of pyrrhotite-rich ore up to a couple of centimetres in thickness are located preferentially near the hanging wall. Chemical analyses show that the Main Orebody is rather homogeneous in composition, with a high bulk sulphide–gangue ratios in relation to the North Orebody. Production from the latter was also higher in zinc and lower in copper than the Main Orebody. The mine was worked to a depth of 1400 m along the dip of the ore, and about 3 Mt with 1.7 % Cu, 5.5 % Zn, 0.4 % Pb and 45 % S was produced during more than 300 years of mining. |
Bibliography: |
From NGU's Reference Archive: |
Vogt, J.H.L. |
Killingdal gruve. |
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 2555;3 pages |
Abstract: | |
Rapporten er en tysk rapport med fundament i Norges Malmforekomster 1906, og omhandler gruven. |
M.E. , 1907 |
Killingdal Pyrites Mine, Norway. |
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 3691;5 pages |
Abstract: | |
Rapporten er en økonomisk vurdering av forekomsten. |
Aasgaard, Gunnar , 1927 |
Gruber og skjerp i kisdraget Øvre Guldal-Tydal. |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.129;1-196 pages |
Abstract: | |
The occurences described in this paper form a connection between th mining districts around Røros to the south and those around Meråker to the north. The occurences lie in mountain regions partly above the forest line. The list on page 12 contains the names of all known occurrences of whatever size within the district considered. Pl. I is a geological outline map of the district, compiled from maps in the Norwegian Geological Survey. In a geological summary on pages 18-27 it is shown that no pyrite occurrences of economic importance so far have been found in an eastern zone along the Swedish boundary where the rocks consist of hard schist with sparagmites, and igneous rocks. Neither have such occurrences been found in a zone of "Stuedalsskifer" and an other zone of "Gulaskifer" towards west, both indicated on the map. The occurrences of pyrite are chiefly found in connection with fine grained, light green or gravish, partly feldspar bearing schist and in connection with green schists, mostly fine grained hornblende schists. All these zones of schist gnereally strike north and dip west. The pyrite bearing schist lie on both sildes of a large zone of igneous rocks extending from Kjølifjell in the south over Hyllingen and Melshogna to Fangen in the Meråker district in the north. |
Rui, Ingolf J. , 1968 |
Geologiske og petrografiske undersøkelser i traktene rundt Killingdal grube i Ålen, Sør.Trøndelag. Forsøk på å løse genetiske problemer i tilknytning til kismineraliseringen. |
;UiO Geografisk inst.;AVHANDLING |
Birkeland, Anne , 1986 |
Mineralogisk og geokjemisk undersøkelse av Killingdal gruven, Sør-Trøndelag. |
;UiO Geologisk fellesråd;AVHANDLING |
Nilsen, O.; Wolff, Fr.Chr. , 1989 |
Røros og Sveg. Berggrunnskart Røros og Sveg M 1:250 000; trykt i farger |
;Norges geologiske undersøkelse;KART;1 kart pages |
Abstract: | |
Beskrivelsen finnes på kartet. |
References not to be found in NGU's Reference Archive.: |
Rui, I. 1973: Structural Control and Wall Rock Alteration at Killingdal Mine, Central Norwegian Caledonides. Econ. Geology, 68, pp. 859-883. |
Carlsen, Kjell B. 1984: A/S Killingdal Grubeselskap: Vurdering av fremtidig drift. BV7291 |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||
Bh10 N64, 85.5-86.0 | Core |
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Bh10 N64, 88.25-89.0 | Core |
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Bh13 N64,17.85-19.25 | Core |
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Bh8 N64, 49.3-50.0 | Core |
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Bh9 N64, 63.0-64.0 | Core |
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Bh9 N64, 64.0-65.3 | Core |
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Bh9 N64, 66.1-67.0 | Core |
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399862 | Dump |
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399863 | Dump |
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399864 | Dump |
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399865 | Dump |
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399866 | Dump |
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399868 | Dump |
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399869 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Killingdal Nord |
(Object Id: 10030 11,01,00) |
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Location |
County: | Trøndelag | Municipality: | Holtålen (5026) |
Map 1:50000: | Ålen (1720-4) | Map 1:250000: | Røros |
Coordinate system: | EU89-UTM Zone 32 |
East: | 626067 m. | North: | 6965654 m. |
Longitude: | 11.4723680 | Latitude: | 62.7993620 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Zinc | |
Element(s): | Zn Cu Kis |
Resources and production |
Activity: | Test mining | Reserves: | ||
Operating method: | Underground mining | Historical production: |
Photo(s) from the Deposit area: |
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Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0200.01 | Dump |
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ST0200.02 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 5026 - 011 Killingdal |
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# |
Bh10 N64, 85.5-86.0 | Core | 3890 | 45200 | 2120 | 136 | 54 | 22.6 | 67.0 |
Bh10 N64, 88.25-89.0 | Core | 917 | 113000 | 8490 | 84 | 12 | 85.7 | 94.0 |
Bh13 N64,17.85-19.25 | Core | 3900 | 89500 | 5180 | 174 | 18 | 41.1 | 192.0 |
Bh8 N64, 49.3-50.0 | Core | 30100 | 44100 | 1635 | 642 | 11 | 26.8 | 178.0 |
Bh9 N64, 63.0-64.0 | Core | 20900 | 4400 | 106 | 291 | 10 | 22.0 | 288.0 |
Bh9 N64, 64.0-65.3 | Core | 18300 | 33900 | 3400 | 275 | 13 | 35.1 | 226.0 |
Bh9 N64, 66.1-67.0 | Core | 6850 | 210000 | 14900 | 89 | 35 | 74.8 | 232.0 |
ST0200.01 | Dump | 942 | 333 | 46 | 53 | 171 | .7 | 21.0 |
ST0200.02 | Dump | 785 | 705 | 104 | 88 | 299 | .8 | 24.0 |
399862 | Dump | 12000 | 78000 | 4405 | 123 | 23 | 21.9 | 67.0 |
399863 | Dump | 77000 | 19000 | 1074 | 107 | 12 | 19.7 | 68.0 |
399864 | Dump | 22000 | 4048 | 397 | 185 | 15 | 12.7 | 50.0 |
399865 | Dump | 6380 | 69000 | 2101 | 20 | 15 | 16.8 | 107.0 |
399866 | Dump | 1917 | 15000 | 8633 | 45 | 17 | 12.8 | 20.0 |
399868 | Dump | 8315 | 67000 | 5503 | 431 | 52 | 41.4 | 273.0 |
399869 | Dump | 6827 | 102000 | 7436 | 138 | 25 | 64.7 | 93.0 |
------------------ |
Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* |
Bh10 N64, 85.5-86.0 | 2.5 | 4.0 | 441 | 115.5 | 1000 | 4.83 | 6 | 9 | 20 |
Bh10 N64, 88.25-89.0 | 2.5 | 2.0 | 1475 | 277.0 | 90 | 6.09 | 12 | 27 | 116 |
Bh13 N64,17.85-19.25 | 2.5 | 2.0 | 501 | 222.0 | 660 | 17.00 | 5 | 17 | 57 |
Bh8 N64, 49.3-50.0 | 2.5 | .5 | 792 | 87.3 | 70 | 17.40 | 6 | 18 | 40 |
Bh9 N64, 63.0-64.0 | 2.5 | .5 | 290 | 12.6 | 100 | 8.40 | 3 | 3 | 23 |
Bh9 N64, 64.0-65.3 | 2.5 | .5 | 1320 | 75.5 | 60 | 10.75 | 8 | 88 | 54 |
Bh9 N64, 66.1-67.0 | 2.5 | .5 | 1235 | 527.0 | 80 | 5.75 | 26 | 91 | 114 |
ST0200.01 | 12.0 | 38.0 | 319 | 1.6 | 65 | 8.00 | -3 | -3 | |
ST0200.02 | 9.0 | 8.0 | 168 | 4.6 | 56 | 28.00 | -3 | -3 | |
399862 | 149 | 142.2 | 12 | 20.00 | 8 | 30 | |||
399863 | 146 | 51.2 | 27 | 4.00 | 5 | 3 | |||
399864 | 378 | 11.2 | 7 | 24.00 | 7 | 3 | |||
399865 | 156 | 202.4 | 19 | 10.00 | 17 | 19 | |||
399866 | 139 | 33.5 | 36 | 13.00 | 32 | 13 | |||
399868 | 184 | 173.5 | 14 | 18.00 | 16 | 62 | |||
399869 | 222 | 213.0 | 17 | 12.00 | 17 | 180 |
------------------ |
Sample No. | Se* | Ga* | Ge* | In* | S% | V* | Cr* | Mn* | Fe% |
Bh10 N64, 85.5-86.0 | 33.00 | 16.35 | 0.23 | 2.15 | 10.00 | 75 | 27 | 144 | 27.10 |
Bh10 N64, 88.25-89.0 | 28.00 | 9.90 | 0.22 | 7.10 | 10.00 | 4 | 3 | 269 | 37.40 |
Bh13 N64,17.85-19.25 | 48.00 | 24.60 | 0.29 | 3.03 | 10.00 | 50 | 17 | 725 | 33.30 |
Bh8 N64, 49.3-50.0 | 127.00 | 10.05 | 0.51 | 3.62 | 10.00 | 13 | 3 | 127 | 40.60 |
Bh9 N64, 63.0-64.0 | 59.00 | 12.45 | 0.30 | 1.14 | 10.00 | 112 | 14 | 420 | 26.50 |
Bh9 N64, 64.0-65.3 | 50.00 | 9.93 | 0.29 | 2.42 | 10.00 | 25 | 13 | 84 | 29.60 |
Bh9 N64, 66.1-67.0 | 26.00 | 18.60 | 0.20 | 13.75 | 10.00 | 43 | 20 | 1250 | 26.20 |
ST0200.01 | 7.73 | 318 | 54 | 1640 | 15.96 | ||||
ST0200.02 | 11.88 | 185 | 43 | 610 | 26.09 | ||||
399862 | 1 | 165 | 252 | 10.00 | |||||
399863 | 8 | 35 | 784 | 19.50 | |||||
399864 | 2 | 107 | 404 | 10.00 | |||||
399865 | 2 | 118 | 178 | 14.90 | |||||
399866 | 8 | 152 | 78 | 14.60 | |||||
399868 | 7 | 67 | 268 | 10.00 | |||||
399869 | 1 | 48 | 168 | 10.00 |
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Sample No. | Th* | U* | W* | Rb* | Sr* | Y* | Zr* | Nb* | Ta* |
Bh10 N64, 85.5-86.0 | 1.84 | 3.20 | 1 | 35.9 | 8.9 | 10.8 | 113 | 0.60 | 0.05 |
Bh10 N64, 88.25-89.0 | 0.03 | 0.40 | 1 | 1.3 | 0.8 | 0.3 | 1 | 0.05 | 0.03 |
Bh13 N64,17.85-19.25 | 2.35 | 2.40 | 1 | 20.4 | 22.5 | 13.6 | 76 | 1.50 | 0.09 |
Bh8 N64, 49.3-50.0 | 0.43 | 0.80 | 1 | 5.4 | 2.7 | 1.1 | 13 | 0.30 | 0.03 |
Bh9 N64, 63.0-64.0 | 0.67 | 0.70 | 1 | 22.5 | 24.7 | 9.3 | 63 | 2.00 | 0.12 |
Bh9 N64, 64.0-65.3 | 0.39 | 0.80 | 1 | 6.0 | 1.6 | 0.7 | 8 | 0.10 | 0.03 |
Bh9 N64, 66.1-67.0 | 1.51 | 0.70 | 1 | 17.6 | 33.9 | 5.2 | 15 | 0.60 | 0.05 |
ST0200.01 | 8.00 | -8.00 | -2 | 15.0 | |||||
ST0200.02 | 8.00 | -8.00 | -2 | 7.0 | |||||
399862 | 3.0 | ||||||||
399863 | 4.0 | ||||||||
399864 | 4.0 | ||||||||
399865 | 3.0 | ||||||||
399866 | 5.0 | ||||||||
399868 | 5.0 | ||||||||
399869 | 3.0 |
------------------ |
Sample No. | Cs* | La* | Ce* | B* | Li* | Be* | P* | Sc* | Ti* |
Bh10 N64, 85.5-86.0 | 0.27 | 6.60 | 19.05 | 6 | 0 | 90 | 9.00 | 760 | |
Bh10 N64, 88.25-89.0 | 0.05 | 0.25 | 0.35 | 1 | 0 | 5 | 0.10 | 25 | |
Bh13 N64,17.85-19.25 | 0.51 | 5.90 | 13.80 | 7 | 1 | 230 | 2.30 | 550 | |
Bh8 N64, 49.3-50.0 | 0.16 | 0.90 | 2.02 | 3 | 0 | 10 | 0.40 | 70 | |
Bh9 N64, 63.0-64.0 | 0.78 | 4.10 | 11.10 | 10 | 0 | 330 | 15.00 | 3070 | |
Bh9 N64, 64.0-65.3 | 0.08 | 1.90 | 3.02 | 2 | 0 | 5 | 0.80 | 90 | |
Bh9 N64, 66.1-67.0 | 1.19 | 6.30 | 13.30 | 5 | 0 | 120 | 3.00 | 490 | |
ST0200.01 | 64.00 | -3 | |||||||
ST0200.02 | 31.00 | -3 | |||||||
399862 | 0.50 | 30 | |||||||
399863 | 4.00 | 300 | |||||||
399864 | 3.00 | 30 | |||||||
399865 | 6.00 | 30 | |||||||
399866 | 0.50 | 30 | |||||||
399868 | 3.00 | 30 | |||||||
399869 | 0.50 | 30 |
------------------ |
Sample No. | Te* | Hf* | Re* | Tl* | |||||
Bh10 N64, 85.5-86.0 | 0.35 | 3.10 | 0 | 17 | |||||
Bh10 N64, 88.25-89.0 | 0.78 | 0.05 | 0 | 10 | |||||
Bh13 N64,17.85-19.25 | 2.27 | 2.20 | 0 | 27 | |||||
Bh8 N64, 49.3-50.0 | 2.73 | 0.40 | 0 | 11 | |||||
Bh9 N64, 63.0-64.0 | 1.86 | 1.70 | 0 | 16 | |||||
Bh9 N64, 64.0-65.3 | 1.53 | 0.20 | 0 | 15 | |||||
Bh9 N64, 66.1-67.0 | 0.83 | 0.50 | 0 | 28 | |||||
ST0200.01 | |||||||||
ST0200.02 | |||||||||
399862 | |||||||||
399863 | |||||||||
399864 | |||||||||
399865 | |||||||||
399866 | |||||||||
399868 | |||||||||
399869 |
The fact sheet was created on 20.04.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
Copyright © 2024 Geological Survey of Norway |