Norsk versjon
THE ORE DATABASE
Deposit Area 2030 - 087
(Last updated 26.jan.2005)

Name of Deposit Area : Brattli
(Object Id : 2030,087,00,00)

Location
County : Finnmark (20) Municipality : Sør-Varanger (2030)
Map 1:50000: Høybuktmoen (2434-3) Map 1:250000: Kirkenes
Marking point: Longitude: 29.9661410 Latitude: 69.5985500
EU89-UTM Zone 36 (Coordinates IS confirmed)
X-coord: 382010 m. Y-coord: 7724034 m.

Commodity
Main Type: Ferrous metals(Fe, Mn, Ti) Sub Type: Iron
Element(s): Fe
Production
Activity: Exploration Reserves:
Prod. method: Production:
Prod. status: Volume of dump:

Importance
Public: Little Importance (reg. 18.02.2015)
Economical: Minor interest , (Confirmed 26.jan.2005 by Agnes Raaness)

Products
Element/product Crude ore grade or quality
FE_MAG 28 %

Operations
From - To Activity Comments
1958 - 1958 Geology Company/Institution :Dipl.NTH
1984 - 1984 Geology Company/Institution :Prospektering A/S

Mineralization
Era: Archean Period:
Dating: Method:
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: Direction:
Plunge:
Stratigraphic classification of host rock
Era: Archean Period:
Province: Troms-Finnmark Basement Province
Geotec.unit:
Tectonic complex:
Igneous complex:
Group: Bjørnevann Group Formation: Fisketind Formation

Mineralogy
Relationship Mineral Amount
Gangue mineral Amphibole Major mineral (>10%)
Gangue mineral Quartz Major mineral (>10%)
Gangue mineral Calcite Accessory mineral (<1%)
Gangue mineral Garnet Accessory mineral (<1%)
Gangue mineral Epidote Accessory mineral (<1%)
Gangue mineral Apatite Accessory mineral (<1%)
Ore mineral Magnetite Major mineral (>10%)

Lithology:
Relationship Rock Origin
Wall rock Quartzite Sedimentary
Original rock :Sandstone
Metamorphic facies :Amphibolite
Wall rock Hornblende gneiss Extrusive
Original rock :Basalt
Metamorphic facies :Amphibolite

Information(s) in free text format
Free text
Malmen ligger NV for Ørnevatn, i flankene av en kompleks synformstruktur som strekker seg over til Ørnevatnmalmen (FI0261). Malmen er hovedsaklig konsentrert i NV, i to adskilte malmkropper. Det er mulig at malmkonsentrasjonen strekker seg mot dypet mot SØ. Malmen er en god liggmalm av samme type som på Kjellmannsåsen og Ørnevatn, med gehalt 25 - 32 % Fe magn. Malmareal: 8500 m2.

Bibliography:
References not to be found in NGU's Reference Archive.:
A/S Sydvaranger 1985: Gruveplan 1985.


Iversen, E. 1986: Jernmalmer i Sør-Varanger. Int. rapp 1689, Prospektering A/S.


Berge, K. 1986: Brattli-Ørnevann-malmen. Int. rapp.1685, Prospektering A/S.


Brevik, P. 1958: Brattli jernmalmfelt. Diplom NTH.


The fact sheet was created on 18.05.2024

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