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INDUSTRIMINERALDATABASEN
Forekomstområde 1825 - 301
(Sist oppdatert 24.feb.2004)

Navn på deposit area : Rørskardet
(Objekt Id : 1825,301,00,00)

Lokalisering
Fylke : Nordland (18) Kommune : Grane (1825)
Kart 1:50000: Majavatn (1925-3) Kart 1:250000: Mosjøen
Markeringspunkt: Lengdegrad: 13.5755190 Breddegrad: 65.2265030
EU89-UTM Zone 33 (Coordinates NOT confirmed)
X-koord: 433400 m. Y-koord: 7234450 m.

Materialtype
Hovedtype: Olivin Subtype: Ultramafitt (uspes.)

Betydning
Offentlig: Not Assessed (reg. 18.02.2015)
Economical: Ikke vurdert

Mineralization
Era: Period:
Dating: Method:
Genesis: Form:
Main texture: Min. distribution:
Main grain size:
Strike/Dip: Direction:
Plunge:
Stratigraphic classification of host rock
Era: Period:
Province:
Geotec.unit:
Tectonic complex:
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.


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