Skip Nav Destination
Article navigation
Other|
August 01, 1996
Reaction textures in contact-metamorphosed xenoliths; implications for the tectonothermal evolution of the Seiland igneous province, Norwegian Caledonides
Synnove Elvevold;
Synnove Elvevold
University of Tromso, Institute of Biology and Geology, Tromso, Norway
Search for other works by this author on:
Synnove Elvevold
University of Tromso, Institute of Biology and Geology, Tromso, Norway
Helge Reginiussen
Publisher: Deutsche Mineralogische Gesellschaft, Sociedad Española de Mineralogia, Societá Italiana di Mineralogia e Petrologia, Société Francaise de Minéralogie
First Online:
02 Mar 2017
Online Issn: 1617-4011
Print Issn: 0935-1221
GeoRef, Copyright 2004, American Geological Institute.
European Journal of Mineralogy (1996) 8 (4): 777–789.
Article history
First Online:
02 Mar 2017
Citation
Synnove Elvevold, Helge Reginiussen; Reaction textures in contact-metamorphosed xenoliths; implications for the tectonothermal evolution of the Seiland igneous province, Norwegian Caledonides. European Journal of Mineralogy 1996;; 8 (4): 777–789. doi:
Download citation file:
You could not be signed in. Please check your email address / username and password and try again.
Index Terms/Descriptors
- Caledonian Orogeny
- Caledonides
- Cambrian
- chain silicates
- contact metamorphism
- cordierite
- corundum
- Europe
- feldspar group
- Finnmark Norway
- framework silicates
- garnet group
- granulites
- ilmenite
- inclusions
- Lower Cambrian
- metamorphic rocks
- metamorphism
- mineral assemblages
- nesosilicates
- Norway
- orthopyroxene
- orthosilicates
- oxides
- P-T conditions
- Paleozoic
- phase equilibria
- Precambrian
- pyroxene group
- quartz
- ring silicates
- Scandinavia
- Seiland
- silica minerals
- silicates
- spinel
- textures
- upper Precambrian
- Western Europe
- xenoliths
- Seiland igneous province
Latitude & Longitude
Citing articles via
Related Articles
Beneath the Stillwater Complex: Petrology and geochemistry of quartz-plagioclase-cordierite (or garnet)-orthopyroxene-biotite ± spinel hornfels, Mountain View area, Montana
American Mineralogist
High-pressure granulite facies metamorphism (∼1.8 GPa) revealed in silica-undersaturated garnet-spinel-corundum gneiss, Central Maine Terrane, Connecticut, U.S.A.
American Mineralogist
Related Book Content
Uplift of the southeastern Australian lithosphere: Thermal-tectonic evolution of garnet pyroxenite xenoliths from western Victoria
The Crust-Mantle and Lithosphere-Asthenosphere Boundaries: Insights from Xenoliths, Orogenic Deep Sections, and Geophysical Studies
Non-ultrahigh-pressure unit bordering the Sulu ultrahigh-pressure terrane, eastern China: Transformation of Proterozoic granulite and gabbro to garnet amphibolite
Ultrahigh-pressure metamorphism: Deep continental subduction
Imprints of modal metasomatism in the post-Deccan subcontinental lithospheric mantle: petrological evidence from an ultramafic xenolith in an Eocene lamprophyre, NW India
Large Igneous Provinces from Gondwana and Adjacent Regions
High-pressure and ultrahigh-temperature granulite-facies metamorphism of Precambrian high-grade terranes: Case study of the Limpopo Complex
Origin and Evolution of Precambrian High-Grade Gneiss Terranes, with Special Emphasis on the Limpopo Complex of Southern Africa