Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 5026 - 008 Syaosen | |||||
(Object Id: 4400) (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: | 630826 m. | North: | 6966775 m. |
Longitude: | 11.5664600 | Latitude: | 62.8077390 |
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 |
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 | |
1997 - 1997 | Sampling | Company/Institution :NGU |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Genesis: | Volcex | Form: | Lens | |
Main texture: | Structureless | Min. distribution: | Disseminated (<20 % ore minerals) |
Main grain size: | Fine grained (< 1 mm) | Main alteration: | Chloritisation |
Strike/Dip: | Direction: | 125 | ||
Plunge: | 15 |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Ordovician |
Province: | Caledonides | |
Geotec.unit: | Røros Nappe Complex | |
Tectonic complex: | Essandsjø Nappe | |
Igneous complex: |
Group: | Aursund | Formation: | Stugusjø |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Chlorite | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Garnet | Subordinate mineral (1-10%) | |
Gangue mineral | Amphibole | Accessory mineral (<1%) | |
Ore mineral | Chalcopyrite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | biotite-quartz schist | Sedimentary Original rock :Siltstone |
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Metamorphic facies :Greenschist |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Crenulation cleavage | Strike/Dip :302 / 50 | Post-mineralisation ;...Effect :Modifies | |
Wall rock | Schistosity | Strike/Dip :106 / 15 | Post-mineralisation ;...Effect :None |
Information(s) in free text format |
Free text |
Forekomsten består av fire mindre skjerp og synker som ligger vest for elva Sya, omtrent på samme høyde i terrenget like over tregrensen i Skarvbekklia i nordskråningen av Skarvskaftet og Nesjøskarven. Alle skjerpene ligger like nord for en markert skrent i terrenget. De var skjerpet tidlig på 1900-tallet og mindre prøvedrift på kobberkis i kvartsgang ble gjort av Røros Kobberverk (Aasgaard 1927). Hovedforekomsten er også kallt Søosen III og består av en vannfyllt skråsynk med sidevegger 3 x 6 m. En falleferdig brakke står igjen ved synken og rester etter skinnegang ligger utover tippen som har volum på omtrent 150 m3. Sulfidsonen kan sees i NØ-veggen i synken. Den er ca. 0,5 m mektig og består av kobberkis-magnetkis i uregelmessige årer og aggregater og er gjerne tilknyttet kvartslinse sterkt skifrig kloritt-biotitt rik bergart som også fører noe granat og amfibol. |
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 | ||||
ST0197.01 | Dump |
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ST0197.02 | Dump |
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400034 | Dump |
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400035 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Syaosen Midtre |
(Object Id: 9978 8,01,00) |
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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: | 630527 m. | North: | 6966836 m. |
Longitude: | 11.5606530 | Latitude: | 62.8083950 |
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 |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Information(s) in free text format |
Free text |
Syaosen Midtre (Søosen II) ligger ca. 300 m vest for hoveskjerpet og er en 1-2 m dyp, vannfyllt grop. Bløt, klorittrik skifer dominerer. Malmsonen er ikke blottet, men på tippen sees tilsvarende sulfidmineralisering som i hovedskjerpet. Kobberkis aggregater og strenger, gjerne i og rundt kvartslinser i klorittrik skifer. |
Photo(s) from the Deposit area: |
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Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0197.03 | Dump |
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ST0197.04 | Dump |
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400036 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Syaosen Vest |
(Object Id: 9979 8,02,00) |
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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: | 630074 m. | North: | 6966877 m. |
Longitude: | 11.5518040 | Latitude: | 62.8089260 |
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 |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Information(s) in free text format |
Free text |
Syaosen Vest (Søosen I) er et lite, gjengrodd skjerp vest for av en liten bekk. Det er svært overdekket i dette området. Vertsbergarten er mindre klorittrik enn i hovedskjerpet og kan karakteriseres som sandstein. Det er skjerpet på en trolig 20-30 cm mektig, grovkornet kvartsgang med aggregater og strenger av kobberkis. Noe kobberkis finnes også i skifrig sideberg til denne. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0197.05 | Dump |
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ST0197.06 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Syaosen Sør |
(Object Id: 9980 8,03,00) |
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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: | 631538 m. | North: | 6966429 m. |
Longitude: | 11.5801370 | Latitude: | 62.8043820 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu Zn |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Information(s) in free text format |
Free text |
Syaosen Sør (Syosen IV) ligger øst for en større bekk ca. 800 m SØ for hovedforekomsten. I en NØ-vendt brattskråning er det skutt ut i en lengde av 3 m og i en høyde opptil 3,5 m. Nederst i SV-veggen er det blottet en minst 10 cm mektig, kobberkisførende kvartsgang. Lengre oppe i veggen finnes en 20-40 cm bred sone med kobberkis-magnetkis strenger i klorittrik bergart med kvartslinser. Det er også utført mindre arbeid nordvest for skjerpet og antyder at sulfidmineraliseringen kan følges over minst 15 m. Vertsbergarten er en kalkførende biotittskifer med enkelte grovkornete amfibolnåler. |
Photo(s) from the Deposit area: |
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Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0197.07 | Dump |
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ST0197.08 | Dump |
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400030 | Dump |
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400031 | Dump |
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400032 | Dump |
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400033 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 5026 - 008 Syaosen |
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# |
ST0197.01 | Dump | 51562 | 553 | -3 | 59 | 55 | 10.3 | 69.0 |
ST0197.02 | Dump | 30248 | 469 | -3 | 64 | 59 | 6.1 | 36.0 |
ST0197.03 | Dump | 6496 | 311 | -3 | 26 | 40 | 1.8 | 20.0 |
ST0197.04 | Dump | 39754 | 1015 | -3 | 61 | 63 | 11.0 | 51.0 |
ST0197.05 | Dump | 24417 | 115 | 8 | 6 | 5 | 7.5 | 325.0 |
ST0197.06 | Dump | 27063 | 192 | 7 | 21 | 26 | 9.3 | 263.0 |
ST0197.07 | Dump | 30795 | 18260 | 4 | 54 | 94 | 6.3 | 118.0 |
ST0197.08 | Dump | 31528 | 14751 | -3 | 156 | 104 | 6.8 | 72.0 |
400030 | Dump | 11200 | 15700 | 13 | 122 | 82 | 2.8 | 56.0 |
400031 | Dump | 14700 | 7708 | 11 | 41 | 74 | 3.6 | 40.0 |
400032 | Dump | 14200 | 8131 | 13 | 32 | 38 | 3.2 | 37.0 |
400033 | Dump | 35500 | 9239 | 16 | 107 | 98 | 8.0 | 164.0 |
400034 | Dump | 36900 | 592 | 14 | 78 | 65 | 7.1 | 19.0 |
400035 | Dump | 33300 | 421 | 14 | 73 | 63 | 6.7 | 18.0 |
400036 | Dump | 22600 | 568 | 14 | 31 | 32 | 5.5 | 28.0 |
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Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sb* | Bi* | S% |
ST0197.01 | -1.0 | -1.0 | 2 | 3.7 | 65 | -1.00 | 4 | 8 | 6.79 |
ST0197.02 | 2.0 | 13.0 | -2 | 3.2 | 41 | -1.00 | -3 | 6 | 4.20 |
ST0197.03 | -1.0 | 4.0 | 2 | 2.0 | 17 | 2.00 | -3 | 8 | 1.13 |
ST0197.04 | -1.0 | 8.0 | -2 | 7.4 | 78 | 2.00 | -3 | 30 | 5.59 |
ST0197.05 | 7.0 | 3.0 | 3 | 1.5 | 2 | 1.00 | -3 | -3 | 3.07 |
ST0197.06 | 6.0 | 12.0 | -2 | 2.0 | 37 | 1.00 | 3 | 8 | 4.06 |
ST0197.07 | 21.0 | 4.0 | -2 | 82.2 | 15 | 8.00 | -3 | 39 | 8.68 |
ST0197.08 | 2.0 | 1.0 | -2 | 66.9 | 10 | 11.00 | -3 | 40 | 10.81 |
400030 | 16 | 55.6 | 7 | 18.00 | 3 | 47 | |||
400031 | 29 | 41.7 | 3 | 20.00 | 3 | 30 | |||
400032 | 10 | 42.7 | 6 | 15.00 | 3 | 17 | |||
400033 | 10 | 62.1 | 22 | 13.00 | 3 | 56 | |||
400034 | 9 | 2.7 | 44 | 2.00 | 3 | 14 | |||
400035 | 13 | 1.8 | 51 | 1.00 | 3 | 11 | |||
400036 | 8 | 2.8 | 40 | 7.00 | 3 | 10 |
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Sample No. | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* | La* |
ST0197.01 | 86 | 72 | 440 | 14.39 | 7.00 | -8.00 | 2 | 2.0 | 19.00 |
ST0197.02 | 85 | 76 | 438 | 12.74 | 8.00 | -8.00 | -2 | 3.0 | 13.00 |
ST0197.03 | 68 | 73 | 449 | 7.06 | 6.00 | -8.00 | -2 | 2.0 | 9.00 |
ST0197.04 | 84 | 60 | 582 | 12.68 | 6.00 | -8.00 | -2 | 2.0 | 7.00 |
ST0197.05 | 3 | 3 | 58 | 2.84 | -2.00 | -8.00 | -2 | 2.0 | 1.00 |
ST0197.06 | 59 | 64 | 589 | 7.99 | 7.00 | -8.00 | 2 | 2.0 | 7.00 |
ST0197.07 | 91 | 65 | 1237 | 14.66 | 10.00 | -8.00 | -2 | 4.0 | 8.00 |
ST0197.08 | 84 | 66 | 1168 | 16.75 | 9.00 | -8.00 | -2 | 3.0 | 8.00 |
400030 | 89 | 80 | 1342 | 10.00 | 2.0 | 5.00 | |||
400031 | 95 | 80 | 1365 | 10.00 | 2.0 | 1.00 | |||
400032 | 106 | 86 | 1708 | 10.00 | 2.0 | 4.00 | |||
400033 | 69 | 111 | 879 | 10.00 | 3.0 | 3.00 | |||
400034 | 82 | 99 | 502 | 10.00 | 2.0 | 10.00 | |||
400035 | 82 | 115 | 569 | 10.00 | 3.0 | 10.00 | |||
400036 | 74 | 135 | 652 | 10.00 | 2.0 | 5.00 |
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Sample No. | B* | Ti* | |||||||
ST0197.01 | -3 | ||||||||
ST0197.02 | -3 | ||||||||
ST0197.03 | -3 | ||||||||
ST0197.04 | 4 | ||||||||
ST0197.05 | -3 | ||||||||
ST0197.06 | -3 | ||||||||
ST0197.07 | -3 | ||||||||
ST0197.08 | -3 | ||||||||
400030 | 120 | ||||||||
400031 | 120 | ||||||||
400032 | 120 | ||||||||
400033 | 120 | ||||||||
400034 | 240 | ||||||||
400035 | 240 | ||||||||
400036 | 300 |
The fact sheet was created on 24.04.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
Copyright © 2024 Geological Survey of Norway |