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THE ORE DATABASE | |||||
Deposit Area 2030 - 067 | |||||
(Last updated 04.feb.2005) |
Name of Deposit Area : Galsajåkka |
(Object Id : 2030,067,00,00) |
Location |
County : | Finnmark (20) | Municipality : | Sør-Varanger (2030) |
Map 1:50000: | Bøkfjorden (2434-1) | Map 1:250000: | Kirkenes |
Marking point: | Longitude: | 29.2181570 | Latitude: | 69.7523760 |
EU89-UTM Zone 36 | (Coordinates IS confirmed) |
X-coord: | 354011 m. | Y-coord: | 7742781 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 04.feb.2005 by Peter Ihlen) |
Operations |
From - To | Activity | Comments | |
1996 - 1996 | Sampling | Company/Institution :NGU |
Mineralization |
Era: | Archean | Period: | ||
Dating: | Method: | |||
Genesis: | Sedex | Form: | Layer | |
Main texture: | Banded | Min. distribution: | Semi-massive (20-50 % ore minerals) |
Main grain size: | Medium grained (1-3 mm) | Main alteration: |
Strike/Dip: | 130 / 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 | Amphibole | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Garnet | Subordinate mineral (1-10%) | |
Ore mineral | Magnetite | Major mineral (>10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Light grey gneiss | Sedimentary Original rock :Greywacke |
|
Metamorphic facies :Amphibolite | |||
Wall rock | Amphibolite | Extrusive Original rock :Basalt |
|
Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Foliation | Strike/Dip :130 / 70 | Post-mineralisation ;...Effect :None | |
Host rock | Primary layering | Strike/Dip :130 / 70 | Syn-mineralisation ;...Effect :Controls |
Information(s) in free text format |
Free text |
Raskest adkomst fra E6 via sti til hytte ved UTM 588450 7739450, men Klokkarelva er relativt bred og dyp, og Ferdesmyra tildels farlig å krysse, men det er godt mulig. Mineraliseringen er blottet i uttørket elveleie, 10 m SV for elvedele, og ligger i blanding av relativt grovkornig amfibolitt med cm-mektige lyse bånd og m-mektige lag av lysegrå gneis, samt gjennomsettende og tilnærmet konkordante pegmatitter av opptil noen meters mektighet. Den finkornige kvartsbåndede magnetitt-mineraliseringen (prøve 01) er 0.5 m mektig, og 25 m mot SV (20 m over) er det nok en 0.5 m mektig malmhorisont. Mineraliseringen synes å ligge i et annet strukturelt nivå enn den nærliggende Galsaluobbal-mineraliseringen (FI0304) mot SØ. |
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 | ||||
FI0305.01 | Bedrock |
|
NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 2030 - 067 Galsajåkka |
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# |
FI0305.01 | Bedrock | 61 | 38 | -3 | -1 | 3 | -.3 | 2.0 |
------------------ |
Sample No. | Pt# | Pd# | Rh# | As* | Cd* | Ba* | Mo* | Sb* | Bi* |
FI0305.01 | 2.0 | 1.0 | -1.0 | 4 | .2 | 24 | -1.00 | -2 | 6 |
------------------ |
Sample No. | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* | La* |
FI0305.01 | 13 | 7 | 285 | 14.97 | 4.00 | 6.00 | -2 | 3.0 | 9.00 |
------------------ |
Sample No. | B* | ||||||||
FI0305.01 | -3 |
The fact sheet was created on 18.05.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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