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THE ORE DATABASE | |||||
Occurence 5026 - 020 Litlrena | |||||
(Object Id: 4413) (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: | 619024 m. | North: | 6971517 m. |
Longitude: | 11.3385650 | Latitude: | 62.8542970 |
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 Fe Au |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Resources and production |
Activity: | Test mining | Reserves: | ||
Operating method: | Underground mining | Historical production: |
Operations |
From - To | Activity | Comments | |
1883 - 1883 | Test mining | ||
1997 - 1997 | Sampling | Company/Institution :NGU |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Genesis: | Volcex | Form: | ||
Main texture: | Banded | Min. distribution: | Massive (>50 % ore minerals) |
Main grain size: | Very unevenly grained | Main alteration: | Chloritisation |
Strike/Dip: | Direction: | |||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Ordovician |
Province: | Caledonides | |
Geotec.unit: | Trondheim Nappe Complex | |
Tectonic complex: | Meråker Nappe | |
Igneous complex: |
Group: | Fundsjø | Formation: | Hersjø |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Chlorite | Major mineral (>10%) | |
Gangue mineral | Amphibole | Major mineral (>10%) | |
Gangue mineral | Quartz | Subordinate mineral (1-10%) | |
Gangue mineral | Feldspar | Subordinate mineral (1-10%) | |
Ore mineral | Chalcopyrite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Magnetite | Major mineral (>10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Amphibolite | Extrusive Original rock :Basalt |
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Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Schistosity | Strike/Dip :220 / 30 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Forekomsten ligger i gran- og bjørkeskog nord for utmark og på sørsida av elva Litjrena, ca. 300 m for dens sammenløp med Storbekken. Finkornet amfibolitt er blottet ved elva og klorittrik skifer finnes i den ene av to vannfyllte groper. Den største av disse er trolig en skråsynk. Det er imidlertid svært lite malmgeologi å se i området utenom på de relativt store tippene som har samlet volum på omtrent 250 m3. Den dominerende malmtypen består av semi-massiv magnetkis med tynne striper/årer av kobberkis. Magnetkis-kobberkis brekjsemalm med amfibol-klorittrike fragmenter og svært finkornet magnetkis finnes også. Sidebergarten på tippen er i hovedsak finkornet amfibolitt og i mindre mengder klorittskifer og gabbro. I følge Aasgaard (1927) skal det også være påvist en 15 cm mektig sone med arsenkis ved denne forekomsten, men arsenkis ble ikke funnet ved befaringen. To prøver er imidlertid anriket på gull (opptil 3,8 g/t Au). |
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. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0211.01 | Dump |
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ST0211.02 | Dump |
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ST0211.03 | Dump |
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ST0211.04 | Dump |
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400024 | Dump |
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400026 | Dump |
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400029 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Litlrena skjerp |
(Object Id: 10005 20,01,00) |
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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: | 618155 m. | North: | 6971467 m. |
Longitude: | 11.3214540 | Latitude: | 62.8541310 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu As |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0211.05 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 5026 - 020 Litlrena |
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# |
ST0211.01 | Dump | 17001 | 2 | -3 | 339 | 307 | 2.1 | 59.0 |
ST0211.02 | Dump | 14041 | 73 | -3 | 49 | 19 | 3.8 | 3827.0 |
ST0211.03 | Dump | 876 | 14 | -3 | 17 | 10 | .3 | 57.0 |
ST0211.04 | Dump | 14672 | 45 | -3 | 238 | 103 | 2.6 | 1737.0 |
ST0211.05 | Dump | 3249 | 5 | 4 | 224 | 216 | .5 | 37.0 |
400024 | Dump | 6893 | 626 | 18 | 197 | 166 | 1.3 | 75.0 |
400026 | Dump | 29900 | 236 | 13 | 363 | 145 | 6.0 | 548.0 |
400029 | Dump | 19600 | 99 | 1 | 468 | 423 | 2.5 | 37.0 |
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Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sb* | Bi* | S% |
ST0211.01 | 3.0 | 3.0 | -2 | -.2 | 2 | -1.00 | -3 | 3 | 16.31 |
ST0211.02 | 1.0 | -1.0 | -2 | -.2 | 63 | -1.00 | -3 | -3 | 2.16 |
ST0211.03 | 1.0 | -1.0 | -2 | -.2 | 4 | -1.00 | -3 | -3 | .30 |
ST0211.04 | 3.0 | 1.0 | 2 | -.2 | 8 | 1.00 | 3 | -3 | 7.19 |
ST0211.05 | 8.0 | 1.0 | 73 | -.2 | 15 | -1.00 | -3 | 7 | 26.39 |
400024 | 30 | 2.1 | 6 | 2.00 | 3 | 3 | |||
400026 | 18 | 1.2 | 2 | 0.50 | 3 | 3 | |||
400029 | 17 | .1 | 2 | 0.50 | 3 | 3 |
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Sample No. | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* | La* |
ST0211.01 | 1 | 6 | 252 | 26.89 | 3.00 | -8.00 | -2 | 28.0 | 1.00 |
ST0211.02 | 32 | 10 | 414 | 40.43 | 5.00 | -8.00 | -2 | 41.0 | 10.00 |
ST0211.03 | 15 | 27 | 238 | 35.11 | 4.00 | -8.00 | -2 | 20.0 | 1.00 |
ST0211.04 | 7 | 11 | 164 | 38.53 | 4.00 | -8.00 | -2 | 6.0 | -1.00 |
ST0211.05 | 14 | 47 | 141 | 33.26 | 5.00 | -8.00 | -2 | 4.0 | 17.00 |
400024 | 22 | 98 | 307 | 10.00 | 8.0 | 5.00 | |||
400026 | 7 | 26 | 321 | 10.00 | 22.0 | 28.00 | |||
400029 | 8 | 26 | 31 | 10.00 | 0.5 | 0.50 |
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Sample No. | B* | Ti* | |||||||
ST0211.01 | -3 | ||||||||
ST0211.02 | -3 | ||||||||
ST0211.03 | -3 | ||||||||
ST0211.04 | -3 | ||||||||
ST0211.05 | -3 | ||||||||
400024 | 180 | ||||||||
400026 | 60 | ||||||||
400029 | 30 |
The fact sheet was created on 26.04.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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