Norsk versjon | |||||
THE INDUSTRIAL MINERAL DATABASE | |||||
Occurence 1825 - 301 Rørskardet | |||||
(Object Id: 14983) (Last updated: 24.02.2004) |
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Location |
County: | Nordland | Municipality: | Grane (1825) |
Map 1:50000: | Majavatn (1925-3) | Map 1:250000: | Mosjøen |
Coordinate system: | EU89-UTM Zone 33 | (Coordinates NOT confirmed) |
East: | 433400 m. | North: | 7234450 m. |
Longitude: | 13.5755190 | Latitude: | 65.2265030 |
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Resource |
Resource Type: | Olivine | Resource Subtype: | Ultramafic (unspec.) |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Mineralization |
Genesis: | Form: | |||
Main texture: | Min. distribution: |
Main grain size: |
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Plunge: |
Stratigraphic classification of host rock |
Era: | Period: |
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Igneous complex: |
Group: | Formation: |
Bibliography: |
From NGU's Reference Archive: |
Gustavson, Magne , 1973 |
Børgefjell. Beskrivelse til det berggrunnsgologiske gradteigskart J.19 - 1: 100 000 |
;Norges geologiske undersøkelse;KARTBESKRIVELSE; TIDSSKRIFTARTIKKEL;NGU; Skrifter; No.298 ; 8;43 + kart pages |
Abstract: | |
Three main structural units are present: 1. The Precambrian (Svecofennokarelian) basement of the Børgefjell Window. ". Low grade (greenschist facies) Lower Paleozoic rocks belonging to the Seve-Køli Nappe Complex. 3. The higher grade (amphibolite facies) Helgeland Nappe, thrust on top of the low grade rocks. The bedrock lithologies within these units are briefly described. Metasediments, metavolcanics and intrusive igneous rocks are present in the Caledonian part of the sequence. Within the Precambrian, granite and granitic gneiss predominate but metasediments and rocks transitional between gneisses and the metasediments are common. The stratigraphical position of the Caledonian rocks is briefly discussed. |
The fact sheet was created on 23.04.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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