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THE ORE DATABASE
Occurence 5605 - 061 Suddesvuome
(Object Id: 1969)
(Last updated: 04.02.2005)

Location
County: Finnmark Municipality: Sør-Varanger (5605)
Map 1:50000: Bøkfjorden (2434-1) Map 1:250000: Kirkenes
Coordinate system: EU89-UTM Zone 36
East: 346025 m. North: 7743227 m.
Longitude: 29.0111290 Latitude: 69.7518100
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Resource
Resource Type: Ferrous metals(Fe, Mn, Ti) Resource Subtype: Iron
Element(s): Fe
Importance
Raw material meaning: Little Importance (reg. 18.02.2015)

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


Operations
From - To Activity Comments
1996 - 1996 Sampling Company/Institution :NGU

Mineralization
Era: Archean Period:
Genesis: Sedex Form: Layer
Main texture: Banded Min. distribution: Semi-massive (20-50 % ore minerals)
Main grain size: Fine grained (< 1 mm) Main alteration:
Strike/Dip: 100 / 70 Direction:
Plunge:
Stratigraphic classification of host rock
Era: Archean Period:
Province: Troms-Finnmark Basement Province
Geotec.unit:
Tectonic complex:
Igneous complex:
Group: Formation:

Mineralogy
Relationship Mineral Amount
Gangue mineral Quartz Major mineral (>10%)
Gangue mineral Amphibole Subordinate mineral (1-10%)
Gangue mineral Feldspar Subordinate mineral (1-10%)
Ore mineral Magnetite Major mineral (>10%)
Ore mineral Pyrite Accessory mineral (<1%)

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

Structures
Location: Type: Orientation(360 gr.): Relation to min.:
Host rock Foliation Strike/Dip :100 / 70 Post-mineralisation ;...Effect :None
Host rock Primary layering Strike/Dip :100 / 70 Syn-mineralisation ;...Effect :Controls

Information(s) in free text format
Free text
Den finkornige kvartsbåndede magnetitt-mineraliseringen (prøve 01) er blottet på en rygg mellom to små vann. Mineraliseringen er stedvis rusten og 5 m mektig. Den ligger i båndet og boudinert amfibolitt, der mørke amfibolrike boudiner er omgitt av lysere bånd. Også dm-mektige granatrike bånd. Opptil 3 - 4 m mektige pegmatittganger skjærer gjennom amfibolitten. Mineraliseringen kan følges NV-over til høyde 205, og SØ-over til tjernet. I forbindelse med jernmalmen finnes som spredte soner i en 10 - 20 m mektig sone med amfibolittgneis og glimmergneis/øyegneis noe spredt sulfidmineralisering. Denne sonen finnes igjen SØ for tjernet, og den bøyer i østlig og senere ØNØ-lig retning før den ved bekken til vann 150 svinger i SØ-lig retning.

Bibliography:
References not to be found in NGU's Reference Archive.:
Iversen, E. 1989: Kartblad Neiden (2334 II). Feltarbeider 1989. Int. rapp. 2074. Prospektering A/S.

Fieldsamples
Sample No. Sample type Miscellanrous
FI0299.01 Bedrock
Sampler: Wilberg/...Stored: Løkken
Comment: Fine grained, quartz banded mt. min.
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:


Analyse Results
from
Deposit Area 5605 - 061 Suddesvuome

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#
FI0299.01 Bedrock 5 -1 -3 -1 -1 -.3 -1.0
------------------
Sample No. Pt# Pd# Rh# As* Cd* Ba* Mo* Sb* Bi*
FI0299.01 1.0 -1.0 -1.0 6 .3 7 -1.00 3 -2
------------------
Sample No. V* Cr* Mn* Fe% Th* U* W* Sr* La*
FI0299.01 6 4 27 19.26 3.00 -5.00 -2 7.0 -1.00
------------------
Sample No. B*
FI0299.01 -3


The fact sheet was created on 05.05.2024

Questions or comments regarding the fact sheet can be emailed to:
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