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THE ORE DATABASE
Deposit Area 1724 - 018
(Last updated 13.jan.1999)

Name of Deposit Area : Stuvågfjellet
(Object Id : 1724,018,00,00)

Location
County : Nord-Trøndelag (17) Municipality : Verran (1724)
Map 1:50000: Holden (1623-2) Map 1:250000: Namsos
Marking point: Longitude: 10.9337430 Latitude: 64.0688910
EU89-UTM Zone 32 (Coordinates IS confirmed)
X-coord: 594339 m. Y-coord: 7106122 m.

Commodity
Main Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Sub Type: Sulphides
Element(s): Kis Fe
Production
Activity: Exploration Reserves:
Prod. method: Production:
Prod. status: Volume of dump:

Importance
Public: Not Assessed (reg. 18.02.2015)
Economical: Not classified/evaluated

Mineralization
Era: Period:
Dating: Method:
Genesis: Volcex Form: Layer
Main texture: Banded Min. distribution: Disseminated (<20 % ore minerals)
Main grain size: Medium grained (1-3 mm) Main alteration:
Strike/Dip: 25 / 55 Direction: 50
Plunge: 10
Stratigraphic classification of host rock
Era: Period:
Province: Caledonides
Geotec.unit: Seve Nappe Complex
Tectonic complex:
Igneous complex:
Group: Formation:

Mineralogy
Relationship Mineral Amount
Gangue mineral Quartz Major mineral (>10%)
Gangue mineral Amphibole Major mineral (>10%)
Gangue mineral Plagioclase Major mineral (>10%)
Gangue mineral Biotite Major mineral (>10%)
Gangue mineral Potassic feldspar Major mineral (>10%)
Ore mineral Magnetite Major mineral (>10%)
Ore mineral Pyrite Major mineral (>10%)
Ore mineral Chalcopyrite Accessory mineral (<1%)

Lithology:
Relationship Rock Origin
Host rock Amphibolite Extrusive
Original rock :Basalt
Metamorphic facies :Amphibolite
Host rock Granitic gneiss Extrusive
Original rock :Rhyolite
Metamorphic facies :Amphibolite

Structures
Location: Type: Orientation(360 gr.): Relation to min.:
Unknown Foliation Strike/Dip :25 / 55 Post-mineralisation ;...Effect :None
Unknown Fold axis Strike/Dip :50 / 10 Post-mineralisation ;...Effect :Modifies

Information(s) in free text format
Free text
Mineraliseringen er blottet pga. av regulering av Holden, og det er ikke foretatt røskingsarbeider. Mineraliseringen opptrer som en 60 m mektig båndet granittisk gneis (varierer fra fin- til middelskornet) med basiske bånd, og fører svovelkis, magnetitt og spor av kobberkis. Ertsen er anriket i smale bånd og striper i både granittisk gneis (prøve 02) og basiske bånd (prøve 01, 03 og 04). Granat er vanlig og opptrer også i bånd i begge bergartstyper.

Fieldsamples
Sample No. Sample type Miscellanrous
NT0231.01 Bedrock
Sampler :Wilberg, R.
Comment :Mafic band of gneiss with hornblende+garnet+pyrite.
No. of registrated element analyses = 1
NT0231.02 Bedrock
Sampler :Wilberg, R.
Comment :Granitic gneiss with pyrite dissemination.
No. of registrated element analyses = 1
NT0231.03 Bedrock
Sampler :Wilberg, R.
Comment :Mafic band with magnetite, pyrite and chalcopyrite.
No. of registrated element analyses = 1
NT0231.04 Bedrock
Sampler :Wilberg, R.
Comment :Biotite rich band of gneiss with magnetite, pyrite and chalcopyrite.
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:


Analyse Results
from
Deposit Area 1724 - 018 Stuvågfjellet

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#
NT0231.01 Bedrock 118 160 525 16 7 1.8 5.0
NT0231.02 Bedrock 187 177 251 14 6 .9 4.0
NT0231.03 Bedrock 236 61 68 41 8 .1 4.0
NT0231.04 Bedrock 136 59 79 23 7 .2 5.0
------------------
Sample No. Pt# Pd# As* Cd* Ba* Mo* Sb* Bi* S%
NT0231.01 3.0 3.0 2 .9 2 2.00 2 9 .75
NT0231.02 2.0 2.0 2 .2 3 3.00 2 4 .62
NT0231.03 3.0 1.0 2 .2 23 18.00 2 2 15.53
NT0231.04 1.0 1.0 3 .3 70 1.00 2 2 .18
------------------
Sample No. V* Cr* Mn* Fe% Th* U* W* Sr* La*
NT0231.01 40 28 345 2.60 1.00 5.00 1 3.0 6.00
NT0231.02 39 15 383 7.19 2.00 5.00 1 3.0 2.00
NT0231.03 137 30 313 6.39 1.00 5.00 1 2.0 4.00
NT0231.04 175 12 341 3.73 1.00 5.00 1 2.0 3.00
------------------
Sample No. B*
NT0231.01 2
NT0231.02 5
NT0231.03 2
NT0231.04 2


The fact sheet was created on 19.05.2024

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