Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 5514 - 002 Årbostad | |||||
(Object Id: 1337) (Last updated: 09.01.2013) |
|
Location |
County: | Troms | Municipality: | Ibestad (5514) |
Map 1:50000: | Andørja (1332-1) | Map 1:250000: | Narvik |
Coordinate system: | EU89-UTM Zone 33 | (Coordinates NOT confirmed) |
East: | 595058 m. | North: | 7645996 m. |
Longitude: | 17.3674620 | Latitude: | 68.9085360 |
Show on map |
|
Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron | |
Element(s): | Fe P |
Importance |
Raw material meaning: | Little Importance (reg. 18.02.2015) |
Resources and production |
Activity: | Exploration | Reserves: | ||
Operating method: | Historical production: |
Products |
Element/product | Crude ore grade or quality | Reg. date | |
Fe-mag. | 21.9 % | 13.01.1995 | |
P | 1.19-2.5 % | 13.01.1995 |
Mineralization |
Era: | Proterozoic | Period: | Neoproterozoic | |
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: | 0 / 0 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Proterozoic | Period: | Neoproterozoic |
Province: | ||
Geotec.unit: | ||
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Hornblende | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Oligoclase | Major mineral (>10%) | |
Gangue mineral | Biotite | Subordinate mineral (1-10%) | |
Gangue mineral | Garnet | Accessory mineral (<1%) | |
Ore mineral | Magnetite | Major mineral (>10%) | |
Ore mineral | Apatite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Amfibolitt | Extrusive Original rock :Basalt |
|
Metamorphic facies :Amphibolite | |||
Wall rock | Kalkspatmarmor | Sedimentary Original rock :Limestone |
|
Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Unknown | Primary layering | Syn-mineralisation ;...Effect :None | ||
Unknown | Foliation | Syn-mineralisation ;...Effect :None |
Information(s) in free text format |
Free text |
Ved Årbostadtinds østre fjellvegg (579 moh.) opptrer en 15-20 m tykk amfibolitt under en 1-2 m tykk kalkspatmarmor. Amfibolitten inneholder varierende mengder finkornet magnetitt. 5 utsøkt rike prøver viste: 21,9 - 25,0 % Fe-magn. 1,19 - 2,51 % P Forrådsklassifikasjon: Magnetittførende areal Tykkelse Sp. v. Tonnasje Antatt gehalt --------------------------------------------------------------------------- 300000 m2 5 m 3,5 5,25 mill. 20,6 Fe-magn. 1,1 % P --------------------------------------------------------------------------- |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
TR0385.01 | Bedrock |
|
||||
TR0385.02 | Bedrock |
|
NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 5514 - 002 Årbostad |
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# |
TR0385.01 | Bedrock | 24 | 10 | 5 | -1 | 7 | -.3 | -2.0 |
TR0385.02 | Bedrock | 23 | 6 | 3 | -1 | 5 | -.3 | -2.0 |
------------------ |
Sample No. | Pt# | Pd# | Rh# | As* | Cd* | Ba* | Mo* | Sb* | Bi* |
TR0385.01 | -3.0 | -3.0 | -5.0 | 5 | .3 | 285 | -1.00 | -2 | -2 |
TR0385.02 | -3.0 | -3.0 | -5.0 | 7 | -.2 | 22 | -1.00 | -2 | -2 |
------------------ |
Sample No. | S% | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* |
TR0385.01 | .26 | 45 | 18 | 178 | 29.93 | 3.00 | 5.00 | -2 | 369.0 |
TR0385.02 | .27 | 35 | 14 | 150 | 24.15 | 3.00 | 5.00 | -2 | 422.0 |
------------------ |
Sample No. | La* | B* | |||||||
TR0385.01 | 12.00 | -3 | |||||||
TR0385.02 | 8.00 | -3 |
The fact sheet was created on 29.04.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
Copyright © 2024 Geological Survey of Norway |