The Bamble Sector, South Norway: a review

Timo G. Nijland*, Daniel E. Harlov, Tom Andersen

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

21 Citations (Scopus)
173 Downloads (Pure)

Abstract

The Proterozoic Bamble Sector, South Norway, is one of the world's classic amphibolite- to granulite-facies transition zones. It is characterized by a well-developed isograd sequence, with isolated 'granulite-facies islands' in the amphibolite-facies portion of the transition zone. The area is notable for the discovery of CO2-dominated fluid inclusions in the granulite-facies rocks by Jacques Touret in the late 1960's, which triggered discussion of the role of carbonic fluids during granulite genesis. The aim of this review is to provide an overview of the current state of knowledge of the Bamble Sector, with an emphasis on the Arendal-Froland-Nelaug-Tvedestrand area and off shore islands (most prominantly Tromøy and Hisøy) where the transition zone is best developed. After a brief overview of the history of geological research and mining in the area, aspects of sedimentary, metamorphic and magmatic petrology of the Bamble Sector are discussed, including the role of fluids. Issues relevant to current geotectonic models for SW Scandinavia, directly related to the Bamble Sector, are discussed at the end of the review.

Original languageEnglish
Pages (from-to)635-658
Number of pages24
JournalGeoscience Frontiers
Volume5
Issue number5
DOIs
Publication statusPublished - Sep 2014
Externally publishedYes

Bibliographical note

Copyright the Publisher 2014. Version archived for private and non-commercial use with the permission of the author/s and according to publisher conditions. For further rights please contact the publisher.

Keywords

  • Bamble Sector
  • South Norway
  • Charnockite
  • Amphibolite- to granulite-facies transition
  • CO₂
  • Brines
  • Precambrian

Fingerprint

Dive into the research topics of 'The Bamble Sector, South Norway: a review'. Together they form a unique fingerprint.

Cite this