Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 5026 - 026 Svenskmenna | |||||
(Object Id: 4419) (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: | 628568 m. | North: | 6968942 m. |
Longitude: | 11.5238910 | Latitude: | 62.8279710 |
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): | Kis Cu Zn |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Resources and production |
Activity: | Mining | Reserves: | ||
Operating method: | Underground mining | Historical production: | 8 thousand tons |
Products |
Element/product | Crude ore grade or quality | Reg. date | |
Cu | 1.37 % | 22.11.1994 | |
S | 42.46 % | 22.11.1994 | |
Zn | 1.80 % | 22.11.1994 |
Operations |
From - To | Activity | Comments | |
1870 - 1880 | Pitting | ||
1882 - 1884 | Regular production | Company/Institution :Os-Hommelvikselskapet | |
1912 - 1914 | Test mining | Company/Institution :Verstraete & fils | |
1915 - 1918 | Regular production | Company/Institution :A. Huitfeldt & Co. |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Genesis: | Sedex | Form: | Plate | |
Main texture: | Porphyroblastic | Min. distribution: | Massive (>50 % ore minerals) |
Main grain size: | Very unevenly grained | Main alteration: | Chloritisation |
Strike/Dip: | 170 / 10 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Cambrian |
Province: | Caledonides | |
Geotec.unit: | Trondheim Nappe Complex | |
Tectonic complex: | Meråkerdekket | |
Igneous complex: |
Group: | Aursund | Formation: | Røsjø |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Chlorite | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Garnet | Accessory mineral (<1%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Pyrite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Subordinate mineral (1-10%) | |
Ore mineral | Magnetite | Accessory mineral (<1%) | |
Ore mineral | Sphalerite | Accessory mineral (<1%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Klorittskifer | Sedimentary Original rock :Argillaceous sediment |
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Metamorphic facies :Greenschist | |||
Wall rock | Sparagmittisk sk. | Sedimentary Original rock :Greywacke |
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Metamorphic facies :Greenschist | |||
Wall rock | Kvartsglimmerskifer | Sedimentary Original rock :Argillaceous sediment |
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Metamorphic facies :Greenschist |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Primary layering | Strike/Dip :220 / 20 | Syn-mineralisation ;...Effect :Controls | |
Host rock | Crenulation cleavage | Post-mineralisation ;...Effect :None |
Information(s) in free text format |
Free text |
Forekomsten ligger i en svakt skrånenede, flat elvedal med Mennaelva i vest og gruveområdet i øst. Idag finnes en stor tipp, rester av gruveutstyret og to inngjerdede sjakter (gjenrast). Området ligger rett østfor en to m høy foss i elva (ca. 100 m). Her finnes en forskifret rustsone <1 m mektig; denne er sikkert en av de få indikasjoner på malm i området. Rett ved denne fossen er det en vannfylt synk (Menna II) i tilknytning til denne rustsonen. Driften var på en <2 m mektig og py-po-cp-malm med gjennomsnittlig mektighet 1/2 - 3/4 m. Det er relativt lite malmstykker på tippen, som domineres av umineralisert klorittisk skifer. Denne bergarten viser dels krenulasjon, ellers homogen. Enkelte prøver med glinsende klorittskifer med 100 % kloritt? I tilknytning til malmen finnes bånd og slirer av klorittstykker, dels gnidd inn i malmen. 3 typer malm ble funnet ved befaringen: - Finkornet py-po-cp-malm, svakt utviklet bånding. Dels noe innblandet kvarts (matriks). Vanligste type . - Grovkornet py-po-malm med < 1 cm store porfyroblastiske py-korn og dels utviklet metamorf tekstur (durchbewegung). Smuldrer lett opp! - Semimassiv, stripet po-cp-malm, uregelmessig i kvartsrik skifer. Remobilisert cp i kvartslinser, evt. på stikk i kloritt (+ po). Malmen er også påtruffet i flere borhull rundt gruveområdet, max. 169 cm kis, ellers noe kisimpregnasjon. |
Photo(s) from the Deposit area: |
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Bibliography: |
From NGU's Reference Archive: |
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. |
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. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||
ST0217.01 | Dump |
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ST0217.02 | Dump |
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ST0217.03 | Dump |
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ST0217.04 | Dump |
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ST0217.05 | Dump |
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ST0217.06 | Dump |
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ST0217.07 | Dump |
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ST0217.08 | Dump |
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399768 | Dump |
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399769 | Dump |
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399770 | Dump |
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399772 | Dump |
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399773 | Dump |
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399774 | Dump |
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399775 | Dump |
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399794 | Dump |
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399795 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Menna II |
(Object Id: 6665 26,01,00) |
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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: | 628418 m. | North: | 6968942 m. |
Longitude: | 11.5209500 | Latitude: | 62.8280240 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Kis Cu Zn |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Name of Locality: Menna III |
(Object Id: 6666 26,02,00) |
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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: | 628419 m. | North: | 6968792 m. |
Longitude: | 11.5208350 | Latitude: | 62.8266790 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Kis Cu Zn |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Analyse Results |
from |
Deposit Area 5026 - 026 Svenskmenna |
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# |
399768 | Dump | 10000 | 1364 | 88 | 220 | 32 | 3.3 | 47.0 |
399769 | Dump | 19000 | 5791 | 83 | 540 | 77 | 6.5 | 44.0 |
399770 | Dump | 5321 | 805 | 22 | 19 | 16 | 2.2 | 45.0 |
399772 | Dump | 12000 | 9707 | 163 | 398 | 37 | 7.4 | 1248.0 |
399773 | Dump | 8965 | 36000 | 314 | 214 | 30 | 9.2 | 113.0 |
399774 | Dump | 3224 | 36000 | 153 | 228 | 28 | 4.1 | 193.0 |
399775 | Dump | 48000 | 2146 | 94 | 16 | 23 | 11.8 | 571.0 |
399794 | Dump | 507 | 349900 | 83600 | 24 | 30 | 136.8 | 198.0 |
399795 | Dump | 3031 | 146900 | 284 | 39 | 41 | 14.2 | 193.0 |
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Sample No. | As* | Cd* | Ba* | Mo* | Sb* | Bi* | V* | Cr* | Mn* |
399768 | 207 | 2.2 | 7 | 13.00 | 3 | 31 | 54 | 131 | 487 |
399769 | 213 | 27.3 | 2 | 16.00 | 3 | 108 | 6 | 110 | 182 |
399770 | 147 | 1.6 | 70 | 6.00 | 3 | 3 | 28 | 243 | 215 |
399772 | 394 | 65.6 | 5 | 16.00 | 3 | 129 | 11 | 152 | 118 |
399773 | 221 | 54.4 | 1 | 12.00 | 3 | 60 | 1 | 138 | 70 |
399774 | 224 | 82.4 | 4 | 11.00 | 3 | 38 | 9 | 118 | 199 |
399775 | 97 | 7.1 | 5 | 10.00 | 3 | 36 | 12 | 156 | 165 |
399794 | 51 | 474.4 | 2 | 13.00 | 35 | 213 | 3 | 52 | 785 |
399795 | 58 | 234.6 | 10 | 15.00 | 3 | 15 | 19 | 154 | 138 |
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Sample No. | Fe% | Sr* | La* | Ti* | |||||
399768 | 10.00 | 7.0 | 10.00 | 120 | |||||
399769 | 10.00 | 3.0 | 0.50 | 30 | |||||
399770 | 7.98 | 7.0 | 7.00 | 180 | |||||
399772 | 10.00 | 4.0 | 0.50 | 60 | |||||
399773 | 10.00 | 3.0 | 0.50 | 30 | |||||
399774 | 10.00 | 4.0 | 2.00 | 30 | |||||
399775 | 10.00 | 3.0 | 1.00 | 120 | |||||
399794 | 15.86 | 4.0 | 0.50 | 60 | |||||
399795 | 16.37 | 12.0 | 3.00 | 240 |
The fact sheet was created on 25.04.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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