(Last updated: 26.01.2005)
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Norsk versjon | ||||
| THE ORE DATABASE | |||||
| Occurence 5605 - 088 Furuneset | |||||
| (Object Id: 1996) (Last updated: 26.01.2005) |
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| Location |
| County: | Finnmark | Municipality: | Sør-Varanger (5605) |
| Map 1:50000: | Høybuktmoen (2434-3) | Map 1:250000: | Kirkenes |
| Coordinate system: | EU89-UTM Zone 36 |
| East: | 382718 m. | North: | 7723060 m. |
| Longitude: | 29.9855480 | Latitude: | 69.5901410 |
| Show on map |
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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: |
Products |
| Element/product | Crude ore grade or quality | Reg. date | |
| Fe-mag. | 30 % | 23.12.1996 |
Operations |
| From - To | Activity | Comments | |
| 1968 - 1968 | Geophysics | Company/Institution :NGU | |
| 1983 - 1983 | Geology | Company/Institution :Prospektering A/S |
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: | 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 | Quartz | Major mineral (>10%) | |
| Gangue mineral | Amphibole | Major mineral (>10%) | |
| Ore mineral | Magnetite | Major mineral (>10%) |
Lithology: |
| Relationship | Rock | Origin | |
| Wall rock | Hornblende gneiss | Extrusive Original rock :Basalt |
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| Metamorphic facies :Amphibolite |
Information(s) in free text format |
| Free text |
| På Furuneset er det flere tynne malmsoner av god kvalitet som ligger i en synform som kommer fra Langfjorden. Blottet malmareal er meget beskjedent, men heikoptermålinger (fra 1968) gir en kraftig anomali som strekker seg ut i Ørnevatn. Den har sannsynligvis sin årsak i større malmmengder på dypere nivå. Eventuell drift her vil ikke kunne skje uten tapping av Ørnevatn. |
Bibliography: |
| References not to be found in NGU's Reference Archive.: |
| Iversen, E. 1985: Muligheter for skjulte driftsaktuelle malmer i malmfeltet, Bjørnevatn. Int. rapp. 1535. Prospektering A/S. |
| Iversen, E. 1985: Jernmalmer i Sør-Varanger. Int. rapp. 1689. Prospektering A/S. |
| The fact sheet was created on 04.05.2024 |
| Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
| Copyright © 2024 Geological Survey of Norway |