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THE ORE DATABASE
Occurence 4211 - 010 Vekselmyr
(Object Id: 5290)
(Last updated: 18.06.2001)

Location
County: Agder Municipality: Gjerstad (4211)
Map 1:50000: Gjerstad (1612-1) Map 1:250000: Arendal
Coordinate system: EU89-UTM Zone 32
East: 502280 m. North: 6523199 m.
Longitude: 9.0395120 Latitude: 58.8486500
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Resource
Resource Type: Precious metals (Au,Ag,PGE) Resource Subtype: Gold
Element(s): Au As Cu
Importance
Raw material meaning: Little Importance (reg. 18.02.2015)

Resources and production
Activity: Pitting Reserves:
Operating method: Historical production:


Operations
From - To Activity Comments
1984 - 1984 Geology Company/Institution :ARCO
1984 - 1984 Geochemistry Company/Institution :ARCO
2000 - 2000 Sampling Company/Institution :NGU

Mineralization
Era: Proterozoic Period: Mesoproterozoic
Genesis: Hydrothermal vein Form: Lens
Main texture: Fracture filling Min. distribution: Disseminated (<20 % ore minerals)
Main grain size: Medium grained (1-3 mm) Main alteration: Sericitisation
Strike/Dip: 60 / 60 Direction:
Plunge:
Stratigraphic classification of host rock
Era: Proterozoic Period: Mesoproterozoic
Province: South Norwegian Basement Province
Geotec.unit: Bamble Complex
Tectonic complex:
Igneous complex:
Group: Formation:

Mineralogy
Relationship Mineral Amount
Gangue mineral Quartz Major mineral (>10%)
Gangue mineral Feldspar Subordinate mineral (1-10%)
Ore mineral Arsenopyrite Major mineral (>10%)
Ore mineral Pyrite Major mineral (>10%)
Ore mineral Chalcopyrite Subordinate mineral (1-10%)

Lithology:
Relationship Rock Origin
Wall rock Amphibolite Extrusive
Original rock :Basalt
Metamorphic facies :Amphibolite

Structures
Location: Type: Orientation(360 gr.): Relation to min.:
Wall rock Foliation Strike/Dip :55 / 65 Pre-mineralisation ;...Effect :None
Wall rock Schistosity Strike/Dip :58 / 55 Syn-mineralisation ;...Effect :Modifies

Information(s) in free text format
Free text
Skjerpet ligger 1 km sørvest for Byholt på sørsida av Gjerstadvatnet. Det består av en liten, 1 x 2 m, utsprengt grunn grop og avrøsket fjell i en lengde av ca. 12 m og med bredde opptil 4 m. Røskingsarbeidene ble utført av ARCO Norway Inc. i 1984. Mindre røskegrøfter på tvers av strøket er nå knapt synlige. En opptil 0,5 m bred kvartsgang med retning 60°/60° kan følges i amfibolitt i hele røskens lengde. Gangen skjærer foliasjonen i amfibolitten (55°/65°) med liten vinkel. Sulfidmineralene utgjør opptil 50 % av gangmassen og består i hovedsak av arsenkis og pyritt med spor av kobberkis og opptrer som aggregater og smale bånd (prøve .01). Kvarts, feltspat med laminer av kloritt og glimmer er gangmineralene. Amfibolitten er dels serisittisert og silfisert med svak sulfidmineralisering rundt gangen (prøve .02). I tillegg finnes mindre umineraliserte slirer og årer med kvarts±granat i denne.

Photo(s) from the Deposit area:
Photo no. 1 showing Mineralisert gang i Vekselmyr"

Bibliography:
From NGU's Reference Archive:
Grahl-Madsen, Laila; Bech, Lone , 1984
Exploration in the Espelandsmyr-Gjerstad area, 1984
;Norges geologiske undersøkelse;RAPPORT;Bergarkivet; No.BA 7970;38 + kart pages
Abstract:
Også som ARCO report, no. 84-23-38 i NGU Dagbokarkivet. The Espelandsmyr-Gjerstad area is part of the Proterozoic Bamble belt. The rocks are in amphibolite or locally granulite metamorphic facies. The orientation of rocks is northeast-southwest with a steep southeast dip. Uncertain facing evidences indicate younging towards the east. The Espelandsmyr-Gjerstad area comprises a mixed volcanic-sedimentary rock package with exhalative features and a few younger granitic and gabbroic intrusives. The mineral occurrences in the area include: a) a stratabound Pb-Zn-Ag massive sulfide deposit of exhalative origin b) stratabound graphite and disseminated Fe-(Cu)-sulfides c) an epigenic As-Au-Cu vein deposit. None of the explored mineral occurrences has been og economic size or grade. The area still has a potential for both epigenetic and stratabound Au deposits.

Fieldsamples
Sample No. Sample type Miscellanrous
AA0118.01 Bedrock
Sampler: J.S. Sandstad/...Stored: Løkken
Comment: Arsenkis-pyritt-kobberkis strenger i grovkornet kvartsåre i grå, finkornet gneis med kloritt/glimmer laminer.
No. of registrated element analyses = 1
AA0118.02 Bedrock
Sampler: J.S. Sandstad/...Stored: Løkken
Comment: Svak pyritt disseminasjon i finkornet kvartsrik bergart (silifisert amfibolitt?).
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:


Analyse Results
from
Deposit Area 4211 - 010 Vekselmyr

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#
AA0118.01 Bedrock 881 29 14 1140 199 1.4 5925.0
AA0118.02 Bedrock 309 33 2 27 38 .2 40.0
------------------
Sample No. Pt# Pd# As* Cd* Ba* Mo* Sb* Bi* S%
AA0118.01 1.0 1.0 99999 .8 29 6.00 9 8 10.70
AA0118.02 1.0 2.0 744 .1 48 6.00 2 2 1.84
------------------
Sample No. V* Cr* Mn* Fe% Th* U* W* Sr* La*
AA0118.01 188 75 101 23.23 3.00 26.00 8 8.0 7.00
AA0118.02 123 86 189 6.17 3.00 4.00 1 9.0 10.00
------------------
Sample No. B*
AA0118.01 22
AA0118.02 2


The fact sheet was created on 28.04.2024

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