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THE ORE DATABASE
Occurence 4032 - 003 Slystøyl
(Object Id: 5558)
(Last updated: 28.03.2020)

Location
County: Telemark Municipality: Fyresdal (4032)
Map 1:50000: Dalen (1513-4) Map 1:250000: Sauda
Coordinate system: EU89-UTM Zone 32
East: 436196 m. North: 6576622 m.
Longitude: 7.8788730 Latitude: 59.3235930
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Resource
Resource Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Resource Subtype: Copper
Element(s): Kis Cu
Importance
Raw material meaning: Little Importance (reg. 18.02.2015)

Resources and production
Activity: Test mining Reserves:
Operating method: Open pit mining Historical production:


Operations
From - To Activity Comments
1541 - 1549 Test mining Company/Institution :Moisesberg Kobberverk
Noe usikkert om driften er fra denne perioden eller seinere (se Berg, 2006)

Mineralization
Era: Proterozoic Period: Neoproterozoic
Genesis: Hydrothermal vein Form:
Main texture: Min. distribution: Irregular (scattered)
Main grain size: Very unevenly grained Main alteration:
Strike/Dip: Direction:
Plunge:
Stratigraphic classification of host rock
Era: Proterozoic Period: Mesoproterozoic
Province: South Norwegian Basement Province
Geotec.unit: Telemark Supergroup
Tectonic complex:
Igneous complex:
Group: Bandak Group Formation:

Mineralogy
Relationship Mineral Amount
Gangue mineral Quartz Major mineral (>10%)
Gangue mineral Muscovite Subordinate mineral (1-10%)
Gangue mineral Feldspar Subordinate mineral (1-10%)
Ore mineral Bornite Major mineral (>10%)

Lithology:
Relationship Rock Origin
Host rock Granite pegmatite Intrusive
Original rock :Granite pegmatite
Wall rock Greenstone Extrusive
Original rock :Basalt

Structures
Location: Type: Orientation(360 gr.): Relation to min.:
Host rock Hydrothermal vein Strike/Dip :280 / 45
Wall rock Foliation Strike/Dip :340 / 40

Information(s) in free text format
Free text
Forekomsten befinner seg i tett granskog i lia om lag 370 m NV for Slystøyl. Forekomsten drevet med en ca. 6 m lang skjæring i ØSØ-VNV retning. Den er 1-1.5 m dyp og inntil 1 m bred. Skjæringen er dels vannfylt, så det er vanskelig å vite hvor dyp den egentlig er. Tipphaugen er totalt overgrodd. Mineralisering består av bornitt tilknyttet en kvartsdominert åre i en 0.5 m mektig granittisk pegmatitt. Det er også svak disseminasjon i pegmatitten. Pegmatitten inneholder grønnlig muskovitt. Retningen på pegmatitten er 280/45, mens foliasjon i omgivende grønnstein er 340/40.

Bibliography:
References not to be found in NGU's Reference Archive.:
Berg, B.I., 2006: Moisesberg i Fyresdal 1541-1549. Norsk Bergverksmuseums undersøkelser av et kobberbergverk i Telemark. Novus forlag og Norsk Bergverksmuseum, Oslo 2006. 400 sider.

Fieldsamples
Sample No. Sample type Miscellanrous
TE0172.01 Dump
Sampler: J.S. Sandstad
Comment: Svært svak bornitt disseminasjon i grovkornet kvarts-feltspat pegmatitt og bornitt-strenger i renere kvartsåre
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:


Analyse Results
from
Deposit Area 4032 - 003 Slystøyl

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#
TE0172.01 Dump 9890 -100 -100 -10 -10 28.0 180.0
------------------
Sample No. Pt# Pd# As* Cd* Mo* Sb* Bi* Cr* Mn*
TE0172.01 -10.0 -10.0 -100 -10.0 -10.00 -10 100 10 300
------------------
Sample No. Fe% W* Sr* Na* Mg* Al* P* Ca* Hg*
TE0172.01 .66 -10 10.0 900 500 2700 60 7100 -10


The fact sheet was created on 24.04.2024

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