Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 5031 - 006 Sandsve | |||||
(Object Id: 4475) (Last updated: 11.01.2022) |
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Location |
County: | Trøndelag | Municipality: | Malvik (5031) |
Map 1:50000: | Stjørdal (1621-1) | Map 1:250000: | Trondheim |
Coordinate system: | EU89-UTM Zone 32 |
East: | 593565 m. | North: | 7021374 m. |
Longitude: | 10.8671470 | Latitude: | 63.3089540 |
Show on map |
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Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Sulphides | |
Element(s): | Kis |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Resources and production |
Activity: | Test mining | Reserves: | ||
Operating method: | Historical production: |
Operations |
From - To | Activity | Comments | |
1990 - 1990 | Sampling | Company/Institution :H. Karlstrøm |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Genesis: | Volcex | Form: | ||
Main texture: | Min. distribution: | Semi-massive (20-50 % ore minerals) |
Main grain size: | Medium grained (1-3 mm) | 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: | Støren Nappe | |
Igneous complex: |
Group: | Støren Group | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Chlorite | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Actinolite | Major mineral (>10%) | |
Gangue mineral | Biotite | Subordinate mineral (1-10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Pyrite | Major mineral (>10%) | |
Ore mineral | Magnetite | Subordinate mineral (1-10%) | |
Ore mineral | Chalcopyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Greenstone | Extrusive Original rock :Basalt |
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Metamorphic facies :Greenschist |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Foliation | Strike/Dip :255 / 50 | Post-mineralisation ;...Effect :Controls | |
Host rock | Mineral lineation | Dir./Plunge :60 / 40 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Sandsvegruva befinner seg en knapp kilometer nordøst for Selbuvegen, drøy 100 m øst for Svetjønna. Gruva består av en stoll som går i sørlig retning inn i åsen. Stollen er ca. 20 m lang med et lite tverrslag mot øst 8 m inne i gruva. Det er en tipp på om lag 120 kbm foran gruveåpningen. I stollåpningen er det en svært skifrig klorittskifer med en utpreget lineasjon (060/40) og foliasjon (255/50). Enkelte cm-tykke striper med pyritt (semimassiv), ellers svært rustent. Mineralisering på tipphaugen består vesentlig av pyritt og magnetkis i rik impregnasjon i matriks dominert av kvarts og aktinolitt, lokalt også en god del kobberkis, samt magnetitt. |
Photo(s) from the Deposit area: |
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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 | ||||
HK90-008 | Bedrock |
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HK90-009 | Bedrock |
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HK90-010 | Bedrock |
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HK90-011S | Bedrock |
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SANDSVE-1 | Dump |
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SANDSVE-2 | Dump |
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SANDSVE-3 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Skjerp 1 |
(Object Id: 37459 6,01,00) |
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Location |
County: | Trøndelag | Municipality: | Malvik (5031) |
Map 1:50000: | Stjørdal (1621-1) | Map 1:250000: | Trondheim |
Coordinate system: | EU89-UTM Zone 32 |
East: | 593551 m. | North: | 7021467 m. |
Longitude: | 10.8669220 | Latitude: | 63.3097920 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Sulphides | |
Element(s): | Kis |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Chlorite | Subordinate mineral (1-10%) | |
Ore mineral | Pyrite | Major mineral (>10%) | |
Ore mineral | Magnetite | Major mineral (>10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Greenstone | Extrusive Original rock :Basalt |
|
Metamorphic facies :Greenschist |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Fold axis | Dir./Plunge :60 / 35 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
En liten vannfylt synk, ca4x3 m i omriss med en 20 kbm tipp. Kun svak pyrittimpregnasjon i kvartsrik bergart å finne. Nord for synken er det en kvartsrik sone med svak disseminasjon av magnetitt (susc. 15-25). |
Name of Locality: Skjerp 2 |
(Object Id: 37460 6,02,00) |
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Location |
County: | Trøndelag | Municipality: | Malvik (5031) |
Map 1:50000: | Stjørdal (1621-1) | Map 1:250000: | Trondheim |
Coordinate system: | EU89-UTM Zone 32 |
East: | 593542 m. | North: | 7021502 m. |
Longitude: | 10.8667630 | Latitude: | 63.3101080 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Sulphides | |
Element(s): | Kis |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Information(s) in free text format |
Free text |
Overgrodd, vannfylt synk, 4x2.5 m i omriss. Ingen blotninger og tippen er fullstendig overgrodd. |
Analyse Results |
from |
Deposit Area 5031 - 006 Sandsve |
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# |
HK90-008 | Bedrock | 1183 | 34 | 20 | 69 | 114 | .5 | 55.0 |
HK90-009 | Bedrock | 2292 | 89 | 2 | 11 | 13 | .4 | 9.0 |
HK90-010 | Bedrock | 474 | 25 | 2 | 14 | 10 | .3 | 6.0 |
HK90-011S | Bedrock | 1069 | 42 | 6 | 21 | 34 | .5 | 15.0 |
SANDSVE-1 | Dump | 5020 | 89 | 3 | 83 | 4 | .9 | 16.0 |
SANDSVE-2 | Dump | 24500 | 577 | 10 | 151 | 15 | 3.5 | 141.0 |
SANDSVE-3 | Dump | 11200 | 283 | 12 | 157 | 8 | 4.1 | 126.0 |
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Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* |
HK90-008 | 6.0 | 5.0 | 122 | .2 | 1 | 39.00 | 2 | 27 | |
HK90-009 | 1.0 | 2.0 | 2 | 1.1 | 1 | 1.00 | 2 | 2 | |
HK90-010 | 1.0 | 2.0 | 8 | .2 | 1 | 5.00 | 2 | 2 | |
HK90-011S | 1.0 | 3.0 | 35 | .6 | 1 | 4.00 | 2 | 5 | |
SANDSVE-1 | -5.0 | 1.0 | 33 | .8 | 10 | 27.00 | -1 | -1 | -1 |
SANDSVE-2 | -5.0 | 1.0 | 81 | 5.1 | 40 | 64.00 | -1 | 2 | 2 |
SANDSVE-3 | -5.0 | 1.0 | 84 | 1.7 | 30 | 32.00 | -1 | 2 | 2 |
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Sample No. | Se* | Ga* | Ge* | In* | S% | V* | Cr* | Mn* | Fe% |
HK90-008 | 13.80 | 93 | 34 | 74 | 14.65 | ||||
HK90-009 | .32 | 76 | 95 | 551 | 9.62 | ||||
HK90-010 | .79 | 11 | 9 | 200 | 2.25 | ||||
HK90-011S | 3.04 | 41 | 28 | 313 | 5.42 | ||||
SANDSVE-1 | 96.00 | 2.00 | -1.00 | -1.00 | 21 | 6 | 811 | 25.90 | |
SANDSVE-2 | 153.00 | 2.00 | -1.00 | -1.00 | 12 | 9 | 1020 | 42.20 | |
SANDSVE-3 | 159.00 | -1.00 | -1.00 | -1.00 | 5 | 6 | 273 | 40.50 |
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Sample No. | Th* | U* | W* | Sr* | Nb* | Ta* | La* | B* | P* |
HK90-008 | 2.00 | 5.00 | 1 | 1.0 | 2.00 | 2 | |||
HK90-009 | 1.00 | 5.00 | 1 | 12.0 | 2.00 | 2 | |||
HK90-010 | 1.00 | 5.00 | 1 | 20.0 | 2.00 | 6 | |||
HK90-011S | 1.00 | 5.00 | 1 | 22.0 | 2.00 | 4 | |||
SANDSVE-1 | -1.00 | -1.00 | -1 | -1.00 | -1.00 | 80 | |||
SANDSVE-2 | -1.00 | -1.00 | -1 | -1.00 | -1.00 | 200 | |||
SANDSVE-3 | -1.00 | -1.00 | -1 | -1.00 | -1.00 | 30 |
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Sample No. | Sc* | Ti* | Te* | ||||||
HK90-008 | |||||||||
HK90-009 | |||||||||
HK90-010 | |||||||||
HK90-011S | |||||||||
SANDSVE-1 | -1.00 | -50 | 2.00 | ||||||
SANDSVE-2 | -1.00 | 220 | 3.00 | ||||||
SANDSVE-3 | -1.00 | -50 | 2.00 |
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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