Tectonic regimes and terrane boundaries in the high-grade Sveconorwegian belt of SW Norway, inferred from U–Pb zircon geochronology and geochemical signature of augen gneiss suites-Reference-Cited by-同舟云学术

Tectonic regimes and terrane boundaries in the high-grade Sveconorwegian belt of SW Norway, inferred from U–Pb zircon geochronology and geochemical signature of augen gneiss suites

Published:1998-01 Issue:1 Volume:155 Page:143-154
ISSN:0016-7649
Container-title:Journal of the Geological Society
language:en
Short-container-title:Journal of the Geological Society

Author:

BINGEN BERNARD,VAN BREEMEN OTTO

Publisher

Geological Society of London

Subject

Geology

Reference59 articles.

1. Precambrian multi-stage crustal evolution in the Bamble sector of south Norway: Pb isotopic evidence from a Sveconorwegian deep-seated intrusion;Andersen;Chemical Geology (Isotope Geoscience Section),1994

2. Metamorphism, provenance ages, and source characteristics of Precambrian clastic sediments in the Bamble sector, Southern Norway: Ar, Sr, Nd, and Pb isotope study;Andersen;Petrology,1995

3. Evolution of feldspars at the amphibolite-granulite-facies transition in augen gneisses (SW Norway): geochemistry and Sr isotopes

4. Redistribution of rare earth elements, thorium, and uranium over accessory minerals in the course of amphibolite to granulite facies metamorphism: The role of apatite and monazite in orthogneisses from southwestern Norway

5. K-Rich Calc-Alkaline Augen Gneisses of Grenvillian Age in SW Norway: Mingling of Mantle-Derived and Crustal Components

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