Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 5032 - 012 Røsbekken | |||||
(Object Id: 4485) (Last updated: 05.07.2023) |
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Location |
County: | Trøndelag | Municipality: | Selbu (5032) |
Map 1:50000: | Stjørdal (1621-1) | Map 1:250000: | Trondheim |
Coordinate system: | EU89-UTM Zone 32 |
East: | 603390 m. | North: | 7020890 m. |
Longitude: | 11.0627550 | Latitude: | 63.3019030 |
Show on map |
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Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron | |
Element(s): | Fe Kis |
Importance |
Raw material meaning: | Little Importance (reg. 18.02.2015) |
Resources and production |
Activity: | Test mining | Reserves: | ||
Operating method: | Open pit and underground mining | Historical production: |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Genesis: | Volcex | Form: | Layer | |
Main texture: | Structureless | Min. distribution: | Semi-massive (20-50 % ore minerals) |
Main grain size: | Fine grained (< 1 mm) | Main alteration: |
Strike/Dip: | 350 / 45 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Ordovician |
Province: | Caledonides | |
Geotec.unit: | Trondheim Nappe Complex | |
Tectonic complex: | Gula Complex | |
Igneous complex: |
Group: | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Siderite | Subordinate mineral (1-10%) | |
Ore mineral | Magnetite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Subordinate mineral (1-10%) | |
Ore mineral | Arsenopyrite | Subordinate mineral (1-10%) | |
Ore mineral | Pyrite | Accessory mineral (<1%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Banded quartzite | Sedimentary Original rock :Exhalite |
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Metamorphic facies :Greenschist | |||
Wall rock | Metagrewacke | Sedimentary Original rock :Greywacke |
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Metamorphic facies :Greenschist |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Schistosity | Strike/Dip :310 / 40 | Post-mineralisation |
Information(s) in free text format |
Free text |
Røsbekken ligger nord for gården Røsåsen. Enkel adkomst er via Espvegen opp til gården og langs en traktorvei derfra fram til bekken. Forekomsten er godt skiltet, og en plakat med informasjon om bergarter og jernmalmer i Strandfjellet er satt opp. Gruva ble drevet av Mostadmark jernverk på midten av 1800-tallet. Forekomsten ligger 20 m nord for brua over Røsbekken og består av en 5x5 m vannfylt skråsynk og en opptil 4 m høy skjæring langs vestsida av en knaus. En 0,5 m mektig sone med massiv magnetitt ligger i nedre del av skjæringen og over denne finnes båndet, kvartsitt med slirer og tynne bånd med magnetitt. Totalt er den magnetitt-førende sona ca. 3 m mektig. Over denne dominerer disseminasjon og slirer/bånd av finkornet magnetkis og arsenkis (dels som 4-5 mm lange nåler) i kvartsitten. Denne kan følges få ti-talls meter videre nordover langs knausen. Analyse av arsenkis-mineraliseringen gir 2 g/t gull. Flere årer og ganger med kvarts gjennomsetter kvartsitten og skifrig metagråvakke ligger under den. Tippen er dels utplanert for traktorveien og gjengrodd ned mot bekken. |
Bibliography: |
From NGU's Reference Archive: |
Torske, Tore , 1965 |
Geology of the Mostadmarka and Selbustrand area, Trøndelag. |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.232;1-83 + ka pages |
Abstract: | |
The bedrock of the area consists of metamorphic epiclastic, volcanic, and intrusive rocks of assumed Lower Ordovician age, assigned to, and lithologically matching the rocks of, the Røros, Støren and Lower Hovin Groups of the Trondheim Region. A detailed petrographic description of the rock varieties is given. The metamorphic grade of all rocks corresponds to the Greenschist Facies. - Small ore deposits occur in connection with the volcanic rocks. They comprise pyrite-pyrrhotite ores of the Leksdal Type, mixed pyrite-magnetite ores, and iron oxide ores. - Lithological variations of the sedimentary rocks is tentatively correlated with events during the early periods of the Caledonian Orogeny. - The volcanism within the area seems to have started with a phase of explosive activity, followed by extrusion (mostly submarine) of copious amounts of spilitic lavas; towards the end of the main period of volcanism a new episode of explosive activity has produced what is called the upper pyroclastic horizon, comprising rocks ranging from coarse volcanic breccia to finegrained tuffs. - The intrusive rocks consist mainly of saussurite gabbros and quartz keratophyres. The latter are thought to be intrusive rather than effusive, and evidence is offered to support this. In some places the character of pyroclastic material points to a quartz keratophyre parentage. Thus, quartz keratophyres may have occurred both as intrusive and volcanic rocks. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||||
Røsbekken-1 | Bedrock |
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Røsbekken-2 | Bedrock |
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Røsbekken-3 | Bedrock |
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ST0283.01 | Dump |
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ST0283.02 | Dump |
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ST0283.03 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Røsbekken 2 |
(Object Id: 37493 12,01,00) |
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Location |
County: | Trøndelag | Municipality: | Selbu (5032) |
Map 1:50000: | Stjørdal (1621-1) | Map 1:250000: | Trondheim |
Coordinate system: | EU89-UTM Zone 32 |
East: | 603418 m. | North: | 7020790 m. |
Longitude: | 11.0632490 | Latitude: | 63.3009980 |
Show on map |
|
Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron | |
Element(s): | Fe Kis |
Resources and production |
Activity: | Exploration | Reserves: | ||
Operating method: | Historical production: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Pyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Metagreywacke | Sedimentary Original rock :Greywacke |
|
Metamorphic facies :Greenschist |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Foliation | Strike/Dip :305 / 40 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Ca. 100 m sør for hovedforekomsten går bekken i et mindre stryk på tvers av strøket. Både båndet kvartsitt og skifrig metagråvakke er blottet, men magnetitt-sonen ble ikke påvist. En 20-30 cm mektig sone med massiv, finkornet magnetkis og noe pyritt ble imidlertid prøvetatt. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
Røsbekken-4 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Røsbekken 3 |
(Object Id: 37494 12,02,00) |
|
Location |
County: | Trøndelag | Municipality: | Selbu (5032) |
Map 1:50000: | Stjørdal (1621-1) | Map 1:250000: | Trondheim |
Coordinate system: | EU89-UTM Zone 32 |
East: | 603456 m. | North: | 7020727 m. |
Longitude: | 11.0639860 | Latitude: | 63.3004300 |
Show on map |
|
Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron | |
Element(s): | Fe Kis |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Ore mineral | Magnetite | Major mineral (>10%) | |
Ore mineral | Pyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Banded quartzite | Sedimentary Original rock :Exhalite |
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Metamorphic facies :Greenschist |
Information(s) in free text format |
Free text |
Et mindre, vannfylt skjerp ligger på østsida av bekken ca. 180 m SSØ for hovedforekomsten. Malmsonen er blottet lengst nordvest i skjerpet og er ca. 0,5 m mektig. Den består av finkornet semi-massiv magnetitt i kvartsittisk bergart |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||||
Røsbekken-5 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 5032 - 012 Røsbekken |
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# |
Røsbekken-1 | Bedrock | 13 | 30 | 4 | 5 | 17 | -.1 | 1.0 |
Røsbekken-2 | Bedrock | 9 | 17 | 2 | 3 | 21 | -.1 | 1.0 |
Røsbekken-3 | Bedrock | 34 | 32 | 2 | 2 | 12 | .2 | 1980.0 |
Røsbekken-4 | Bedrock | 333 | 562 | 153 | 19 | 254 | 2.1 | 209.0 |
Røsbekken-5 | Bedrock | 74 | 51 | 9 | 18 | 21 | -.1 | 14.7 |
------------------ |
Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* |
Røsbekken-1 | 2 | -.1 | 96 | 4.80 | -1 | 2 | -0 | ||
Røsbekken-2 | 1 | -.1 | 149 | 1.80 | -1 | 1 | -0 | ||
Røsbekken-3 | -5.0 | 2.0 | 10000 | .1 | 30 | 1.65 | -0 | 12 | 0 |
Røsbekken-4 | 6.0 | 7.0 | 344 | 2.1 | 60 | 133.00 | 1 | 77 | 1 |
Røsbekken-5 | 7 | -.1 | 2291 | 2.10 | -1 | 1 | -0 |
------------------ |
Sample No. | Se* | Ga* | Ge* | In* | S% | V* | Cr* | Mn* | Fe% |
Røsbekken-1 | -0.50 | 4.80 | .04 | 52 | 27.05 | ||||
Røsbekken-2 | -0.50 | 3.30 | .02 | 62 | 20.75 | ||||
Røsbekken-3 | 3.00 | 1.06 | -0.05 | 0.02 | 3.27 | 17 | 13 | 513 | 7.08 |
Røsbekken-4 | 7.00 | 5.36 | 0.06 | 0.05 | 10.00 | 138 | 23 | 483 | 40.80 |
Røsbekken-5 | -0.50 | 6.10 | .98 | 48 | 26.34 |
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Sample No. | Th* | U* | W* | Rb* | Sr* | Y* | Zr* | Nb* | Ta* |
Røsbekken-1 | 0.20 | 0.60 | 1 | 0.6 | 175.7 | 4.1 | 6 | 1.00 | -0.10 |
Røsbekken-2 | -0.20 | 0.50 | -1 | 0.6 | 289.6 | 3.1 | 5 | 1.10 | -0.10 |
Røsbekken-3 | 0.04 | 0.20 | 0 | 1.3 | 5.0 | 1.1 | 1 | 0.10 | -0.05 |
Røsbekken-4 | 2.88 | 8.80 | 1 | 18.2 | 19.6 | 5.5 | 33 | 0.70 | 0.05 |
Røsbekken-5 | 0.90 | 0.60 | 2 | 6.8 | 520.6 | 6.3 | 13 | 2.20 | -0.10 |
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Sample No. | Cs* | La* | Ce* | Pr* | Nd* | Sm* | Eu* | Gd* | Tb* |
Røsbekken-1 | 0.10 | 1.80 | 3.70 | 0.42 | 1.70 | 0.39 | 0.11 | 0.47 | 0.09 |
Røsbekken-2 | 0.30 | 2.70 | 2.80 | 0.39 | 1.60 | 0.31 | 0.09 | 0.41 | 0.07 |
Røsbekken-3 | 0.09 | 0.50 | 0.69 | ||||||
Røsbekken-4 | 1.13 | 8.90 | 18.75 | ||||||
Røsbekken-5 | 0.60 | 5.30 | 10.90 | 1.05 | 3.90 | 0.86 | 0.25 | 0.89 | 0.15 |
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Sample No. | Dy* | Ho* | Er* | Tm* | Yb* | Lu* | Li* | Be* | Na* |
Røsbekken-1 | 0.59 | 0.13 | 0.50 | 0.08 | 0.60 | 0.10 | -1 | ||
Røsbekken-2 | 0.46 | 0.10 | 0.33 | 0.04 | 0.24 | 0.04 | 1 | ||
Røsbekken-3 | 2 | 0 | 100 | ||||||
Røsbekken-4 | 10 | 0 | 500 | ||||||
Røsbekken-5 | 0.97 | 0.23 | 0.70 | 0.11 | 0.67 | 0.10 | 3 |
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Sample No. | Mg* | Al* | P* | K * | Ca* | Sc* | Ti* | Te* | Hf* |
Røsbekken-1 | 218 | 0.10 | |||||||
Røsbekken-2 | 305 | -0.10 | |||||||
Røsbekken-3 | 700 | 1300 | 90 | 300 | 1200 | 0.50 | -50 | 0.72 | -0.10 |
Røsbekken-4 | 1900 | 14800 | 560 | 4900 | 2000 | 4.20 | 320 | 0.74 | 0.80 |
Røsbekken-5 | 305 | 0.30 |
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Sample No. | Re* | Hg* | Tl* | ||||||
Røsbekken-1 | -0 | -0 | |||||||
Røsbekken-2 | -0 | -0 | |||||||
Røsbekken-3 | 0 | 0 | |||||||
Røsbekken-4 | 0 | 0 | |||||||
Røsbekken-5 | -0 | -0 |
Oxide analyses |
( All values are in % ) |
Sample No. | Sample Type | SiO2 | Al2O3 | TiO2 | Fe2O3 | MnO | MgO | CaO |
Røsbekken-1 | Bedrock | 56.09 | 0.67 | 0.02 | 38.67 | 1.26 | 0.14 | 0.40 |
Røsbekken-2 | Bedrock | 68.20 | 0.39 | 0.02 | 29.66 | 0.17 | 0.08 | 0.43 |
Røsbekken-5 | Bedrock | 39.73 | 1.29 | 0.06 | 37.66 | 5.00 | 0.50 | 3.49 |
------------------ |
Sample No. | Na2O | K2O | P2O5 | Sum | |||||
Røsbekken-1 | 0.34 | -0.01 | 0.05 | 98.00 | |||||
Røsbekken-2 | 0.19 | -0.01 | 0.07 | 99.00 | |||||
Røsbekken-5 | 0.05 | 0.15 | 0.07 | 88.00 |
The fact sheet was created on 04.05.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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