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THE ORE DATABASE | |||||
Occurence 5026 - 028 Guldals grube | |||||
(Object Id: 4421) (Last updated: 07.11.2023) |
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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: | 629906 m. | North: | 6970348 m. |
Longitude: | 11.5512170 | Latitude: | 62.8401110 |
Show on map |
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Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu Zn Fe Kis |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Resources and production |
Activity: | Mining | Reserves: | ||
Operating method: | Underground mining | Historical production: | 1 thousand tons |
Operations |
From - To | Activity | Comments | |
1774 - 1779 | Regular production | Company/Institution :Røros Kobberverk | |
1823 - 1823 | Test mining | Company/Institution :Røros Kobberverk | |
1847 - 1848 | Test mining | Company/Institution :Røros Kobberverk og Klinkenbergs interes | |
Det var noe strid om rettighetene i denne perioden. | |||
1905 - 1915 | Test mining | Company/Institution :Flere selskaper | |
Periodevis drift | |||
1997 - 1997 | Sampling | Company/Institution :NGU |
Mineralization |
Era: | Paleozoic | Period: | ||
Genesis: | Volcex | Form: | ||
Main texture: | Breccia cement | Min. distribution: | Massive (>50 % ore minerals) |
Main grain size: | Fine grained (< 1 mm) | Main alteration: | Chloritisation |
Strike/Dip: | Direction: | |||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: |
Province: | Caledonides | |
Geotec.unit: | Røros Nappe Complex | |
Tectonic complex: | ||
Igneous complex: |
Group: | Aursund | Formation: | Røsjø |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Amphibole | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Chlorite | Subordinate mineral (1-10%) | |
Ore mineral | Sphalerite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Magnetite | Major mineral (>10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Sandstone | Sedimentary Original rock :Sandstone |
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Metamorphic facies :Amphibolite | |||
Wall rock | Quartz-biotite schist | Sedimentary Original rock :Greywacke |
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Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Foliation | Strike/Dip :0 / 35 | Post-mineralisation ;...Effect :Modifies | |
Wall rock | Schistosity | Strike/Dip :335 / 45 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Forekomsten ligger ca. 940 moh og omtrent 1 km NØ for Rørosmenna i et småkupert område ved et lite tjern på vestsida av Gauldalsgruvhøgda. Gruveområdet består av en rekke gruveåpninger, skjerp, tipper og rester etter gamle brakker. Forekomsten ble mutet av Røros Kobberverk i 1774 og var i drift fram til 1779. Mindre drift var det i 1823 og senere i 1848. Da sto både Kobberverket og Klinkenbergs Interessentskap bak driften og det var konflikter om rettighetene. Driften ble gjenopptatt i 1906-15 og totalt skal det være tatt ut omkring 1.000 tonn kobbermalm. Hovedgruva ligger på nordsida av en bekk og er drevet som en skråsynk med orientering øst-vest ned til omtrent 27 m under dagen. I følge Aasgaard (1927) skal dette være en kobbermalmgruve med kobberkis og magnetkis i en kvartsgang. På tippene dominerer imidlertid massiv breksjemalm som består av magnetkis og kobberkis og varierende mengder sinkblende, med fragmenter av grønne silikater og runde kvartsøyne. I tillegg finnes også båndet magnetitt, magnetkis og kobberkis malm i denne forekomsten. Kvartsittisk sandstein og kvarts-biotittskifer utgjør sidebergartene, og de er gjerne klorittisert inn mot sulfidsonene. |
Photo(s) from the Deposit area: |
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Bibliography: |
From NGU's Reference Archive: |
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.; Bakke, Inge , 1975 |
Stratabound sulphide mineralization in the Kjøli area, Røros district, Norwegian Caledonides. |
;Norsk geologisk forening;TIDSSKRIFTARTIKKEL;Norsk geologisk tidsskrift; No.55 (1);51-75 pages |
Abstract: | |
Two important sulphide ore-bearing formations have been recognized in the Cambro-Silurian succession of the Røros district. One is composed of submarine greenstones and quartz keratophyres (the Hersjø Formation). The other one, which is studied here, consists of a heterogeneous series of banded meta-argillites and meta-greywackes with subordinate thin green interlayers of probable volcanogenic origin (the Røsjø Formation). These two formations are embedded in a thick succession of various clastic sedimentary rocks which have undergone metamorphism and folding during the Silurian orogeny. The numerous sulphide deposits which occur in the Kjøli area are largely confined to the Røsjø Formation. The sulphide bodies are chiefly composed of massive pyrite and/or pyrrhotite showing variable chalcopyrite and sphalerite grades. The massive sulphides often occur as thin, extensive sheets, locally as irregular, small lenses which rarely exceed one metre in thickness. It is probable that the sulphides have been precipitated primarily on the sea-floor, but there is no clear evidence of a volcanogenic origin. Local discordant relationships between the massive sulphides and the wall rocks are ascribed to metamorphic mobilization of the sulphides. The thicker sulphide lenses may themselves represent mobilized portions of thinner sulphide-rich units. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
Guldal-1 | Dump |
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ST0219.06 | Dump |
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TB-Røros 19-40 | Dump |
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TB-Røros 19-41 | Dump |
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TB-Røros 19-42 | Dump |
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399782 | Dump |
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399783 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Sample point: Guldals grube |
(Object Id: 10018 28,00,01) |
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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: | 629906 m. | North: | 6970283 m. |
Longitude: | 11.5511540 | Latitude: | 62.8395270 |
Show on map |
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Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu Zn Fe Kis |
Information(s) in free text format |
Free text |
På nordsida ev en mindre, vannfyllt synk finnes en ca. 2 m bred malmsone som består av båndet, massiv magnetitt, magnetkis og kobberkis malm. Magnetitt og magnetkis veksler i noen mm-tynne bånd som er gjennomsatt av årer og strenger med kobberkis. |
Photo(s) from the Deposit area: |
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Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0219.03 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
Name of Sample point: Guldals grube |
(Object Id: 10019 28,00,02) |
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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: | 629972 m. | North: | 6970161 m. |
Longitude: | 11.5523580 | Latitude: | 62.8384110 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu Zn Fe Kis |
Information(s) in free text format |
Free text |
I en dagskjæring utenfor stollinngangen til Gammelgruven gjenstår 30-40 cm mektig magnetkis-kobberkis malm som overlagres av biotitt-kloritt rik skifer. I tillegg finnes båndet magnetitt, magnetkis og kobberkis malm på tippen. Malmen i Gammelgruven skal ha vært fattigere på kobberkis enn i Hovedgruven. |
Photo(s) from the Deposit area: |
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Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0219.04 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Sample point: Guldals grube |
(Object Id: 10020 28,00,03) |
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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: | 629956 m. | North: | 6970222 m. |
Longitude: | 11.5520990 | Latitude: | 62.8389570 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu Zn Fe Kis |
Information(s) in free text format |
Free text |
På tipper omkring Tydølernes skjerp dominerer magnetkis-kobberkis breksjemalm. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0219.05 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Guldal skjerp I |
(Object Id: 10021 28,01,00) |
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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: | 629237 m. | North: | 6970191 m. |
Longitude: | 11.5379610 | Latitude: | 62.8389360 |
Show on map |
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Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu Zn Kis |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Amphibole | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Chlorite | Subordinate mineral (1-10%) | |
Ore mineral | Chalcopyrite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Sphalerite | Major mineral (>10%) |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Schistosity | Strike/Dip :82 / 55 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Skjerpet består av en gjenrast og gjenvoskt grop med mindre tipp omkring. Kun svak sulfidmineralisering kan observeres i kloritt-amfibol rik skifer i skjerpet. Rik, magnetkis-kobberkis-sinkblende breksjemalm er prøvetatt fra tipp i området. Denne kan imidlertid også komme fra taubanetransporten fra Kjøli gruve som passerte nær dette området. |
Photo(s) from the Deposit area: |
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Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0219.01 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Guldal skjerp II |
(Object Id: 10022 28,02,00) |
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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: | 629560 m. | North: | 6970253 m. |
Longitude: | 11.5443440 | Latitude: | 62.8393810 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu Zn Fe Kis |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Amphibole | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Chlorite | Subordinate mineral (1-10%) | |
Ore mineral | Sphalerite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Major mineral (>10%) |
Information(s) in free text format |
Free text |
Skjerpet er en røskegrop med vegger 3 x 2 m. Linseformet, opptil 20-30 cm mektig, massiv breksjemalm står igjen i NØ-veggen. Vertsbergarten er en finkornet, grågrønn sandstein og svak klorittisering sees inn mot sulfidsona. |
Photo(s) from the Deposit area: |
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Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
Guldal skjerp-1 | Dump |
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ST0219.02 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 5026 - 028 Guldals grube |
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# |
Guldal skjerp-1 | Dump | 4680 | 23500 | 32 | 136 | 94 | 2.1 | 80.0 |
Guldal-1 | Dump | 26000 | 2550 | 7 | 154 | 62 | 6.8 | 32.0 |
ST0219.01 | Dump | 32576 | 29373 | 12 | 271 | 81 | 11.1 | 49.0 |
ST0219.02 | Dump | 9109 | 27392 | 827 | 170 | 106 | 8.1 | 59.0 |
ST0219.03 | Bedrock | 34107 | 764 | 10 | 199 | 13 | 4.8 | 63.0 |
ST0219.04 | Dump | 5610 | 2168 | 3 | 61 | 15 | 1.9 | 17.0 |
ST0219.05 | Dump | 25452 | 8146 | 13 | 158 | 42 | 7.0 | 52.0 |
ST0219.06 | Dump | 33482 | 12839 | 9 | 231 | 52 | 7.8 | 163.0 |
TB-Røros 19-40 | Dump | 1270 | 32100 | 8 | 414 | 75 | .6 | 13.0 |
TB-Røros 19-41 | Dump | 37700 | 948 | 12 | 63 | 7 | 5.9 | 18.0 |
TB-Røros 19-42 | Dump | 1730 | 142 | 2 | 9 | 1 | 1.1 | .5 |
399782 | Dump | 14000 | 1946 | 72 | 327 | 87 | 2.9 | 64.0 |
399783 | Dump | 13000 | 8871 | 80 | 95 | 26 | 4.7 | 31.0 |
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Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* |
Guldal skjerp-1 | 2.5 | .5 | 1 | 65.6 | 80 | 5.77 | 9 | 0 | 14 |
Guldal-1 | 2.5 | 1.0 | 2 | 6.9 | 120 | 6.52 | 9 | 0 | 19 |
ST0219.01 | -1.0 | -1.0 | 4 | 87.9 | 20 | 4.00 | 7 | 26 | |
ST0219.02 | 3.0 | 2.0 | -2 | 85.9 | 14 | 4.00 | -3 | 59 | |
ST0219.03 | 2.0 | 2.0 | -2 | 1.2 | 2 | 1.00 | 4 | 15 | |
ST0219.04 | 1.0 | -1.0 | -2 | 4.4 | 8 | -1.00 | -3 | -3 | |
ST0219.05 | 2.0 | 2.0 | -2 | 23.3 | 34 | 3.00 | 4 | 12 | |
ST0219.06 | 2.0 | 1.0 | -2 | 37.7 | 28 | 3.00 | 14 | 28 | |
TB-Røros 19-40 | 2.5 | .5 | 1 | 76.6 | 10 | 9.83 | 2 | 0 | 19 |
TB-Røros 19-41 | 2.5 | .5 | 1 | 2.9 | 20 | 5.14 | 14 | 0 | 7 |
TB-Røros 19-42 | 2.5 | .5 | 1 | .1 | 10 | 0.69 | 4 | 0 | 4 |
399782 | 87 | 6.6 | 13 | 16.00 | 3 | 28 | |||
399783 | 176 | 23.9 | 9 | 8.00 | 3 | 3 |
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Sample No. | Se* | Ga* | Ge* | In* | S% | V* | Cr* | Mn* | Fe% |
Guldal skjerp-1 | 49.00 | 14.70 | 0.45 | 2.00 | 10.00 | 82 | 54 | 1050 | 31.40 |
Guldal-1 | 45.00 | 25.80 | 0.74 | 2.19 | 7.37 | 82 | 60 | 1030 | 32.30 |
ST0219.01 | 29.10 | 23 | 45 | 360 | 38.46 | ||||
ST0219.02 | 22.76 | 22 | 44 | 342 | 34.62 | ||||
ST0219.03 | 15.51 | 3 | 1 | 91 | 43.14 | ||||
ST0219.04 | 5.04 | 38 | 11 | 363 | 40.39 | ||||
ST0219.05 | 17.08 | 57 | 59 | 586 | 28.89 | ||||
ST0219.06 | 18.35 | 41 | 45 | 405 | 34.51 | ||||
TB-Røros 19-40 | 96.00 | 10.95 | 0.63 | 8.03 | 10.00 | 2 | 2 | 185 | 50.00 |
TB-Røros 19-41 | 36.00 | 19.95 | 1.95 | 2.44 | 4.47 | 19 | 19 | 687 | 41.30 |
TB-Røros 19-42 | 4.00 | 41.90 | 1.50 | 0.73 | .27 | 11 | 9 | 134 | 50.00 |
399782 | 50 | 77 | 433 | 10.00 | |||||
399783 | 23 | 23 | 202 | 10.00 |
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Sample No. | Th* | U* | W* | Rb* | Sr* | Y* | Zr* | Nb* | Ta* |
Guldal skjerp-1 | 4.15 | 1.50 | 0 | 4.9 | 64.4 | 12.2 | 29 | 5.20 | 0.39 |
Guldal-1 | 4.63 | 1.70 | 0 | 186.0 | 13.8 | 17.0 | 39 | 7.00 | 0.48 |
ST0219.01 | 5.00 | -8.00 | 6 | 2.0 | |||||
ST0219.02 | 7.00 | -8.00 | 5 | 3.0 | |||||
ST0219.03 | 5.00 | -8.00 | -2 | 1.0 | |||||
ST0219.04 | 5.00 | -8.00 | -2 | 1.0 | |||||
ST0219.05 | 6.00 | -8.00 | 3 | 3.0 | |||||
ST0219.06 | 6.00 | -8.00 | -2 | 2.0 | |||||
TB-Røros 19-40 | 0.09 | 0.50 | 0 | 0.2 | 1.4 | 1.1 | 2 | 0.20 | 0.03 |
TB-Røros 19-41 | 4.06 | 1.20 | 0 | 9.2 | 28.4 | 59.3 | 69 | 5.70 | 0.37 |
TB-Røros 19-42 | 0.46 | 0.10 | 0 | 2.2 | 0.6 | 0.6 | 2 | 1.00 | 0.09 |
399782 | 7.0 | ||||||||
399783 | 2.0 |
------------------ |
Sample No. | Cs* | La* | Ce* | B* | Li* | Be* | Sc* | Ti* | Te* |
Guldal skjerp-1 | 1.06 | 12.10 | 30.20 | 13 | 1 | 10.60 | 1631 | 5.88 | |
Guldal-1 | 39.60 | 9.40 | 24.90 | 6 | 1 | 11.50 | 1733 | 9.95 | |
ST0219.01 | 5.00 | -3 | |||||||
ST0219.02 | 7.00 | -3 | |||||||
ST0219.03 | -1.00 | -3 | |||||||
ST0219.04 | 4.00 | -3 | |||||||
ST0219.05 | 11.00 | -3 | |||||||
ST0219.06 | 10.00 | -3 | |||||||
TB-Røros 19-40 | 0.05 | 0.25 | 0.77 | 0 | 0 | 0.20 | 60 | 6.24 | |
TB-Røros 19-41 | 9.49 | 14.90 | 36.30 | 6 | 5 | 6.50 | 1830 | 3.03 | |
TB-Røros 19-42 | 0.42 | 0.25 | 0.82 | 0 | 0 | 0.90 | 470 | 0.86 | |
399782 | 11.00 | 360 | |||||||
399783 | 0.50 | 180 |
------------------ |
Sample No. | Hf* | Re* | Tl* | ||||||
Guldal skjerp-1 | 0.80 | 0 | 0 | ||||||
Guldal-1 | 1.00 | 0 | 2 | ||||||
ST0219.01 | |||||||||
ST0219.02 | |||||||||
ST0219.03 | |||||||||
ST0219.04 | |||||||||
ST0219.05 | |||||||||
ST0219.06 | |||||||||
TB-Røros 19-40 | 0.10 | 0 | 0 | ||||||
TB-Røros 19-41 | 1.40 | 0 | 0 | ||||||
TB-Røros 19-42 | 0.10 | 0 | 0 | ||||||
399782 | |||||||||
399783 |
The fact sheet was created on 18.04.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
Copyright © 2024 Geological Survey of Norway |