Sulitjelmafeltet. Berggrunnsgeologisk kart - M 1 : 100 000. Beskrivelse.

The eugeoclinal rocks of the Sulitjelma region occup a large depression in the Norwegian Caldonodrd betwwen the Nasafjell tectonic window of Precambrian rocks in the south and the Tysfjord window in the north. The age of the rocks is thought to be Cambro-Silurian. The regionl metamophism is mainly i...

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Bibliographic Details
Main Author: Kollung, Sigbjørn
Format: Map
Language:Norwegian
Published: 1989
Subjects:
OFIOLITT
GRØNNSTEIN
KALEDONSKE FJELLKJEDE
MALMFOREKOMST
REGIONAL KARTLEGGING
STRATIGRAFI
Norway
Sulitjelma
Tysfjord
Fauske
Junkerdal
Lønsdal
Låmivatnet
Balvatnet
Online Access:https://hdl.handle.net/11250/2674398
Description
Summary:The eugeoclinal rocks of the Sulitjelma region occup a large depression in the Norwegian Caldonodrd betwwen the Nasafjell tectonic window of Precambrian rocks in the south and the Tysfjord window in the north. The age of the rocks is thought to be Cambro-Silurian. The regionl metamophism is mainly in greenschist facies in the lower units, amphibolite facies in the Gasak Nappe and greenschist to amphibolite facies in the Fauske Nappe. Some of the largest sulphide deposits in Norway are located near Sulitjelma. The different types of mineralizations occurring in the region are briefly described. 35684

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