Skip Nav Destination
Article navigation
Other|
June 01, 1993
The reconstructive 2/1- to 3/2-mullite transformation in the presence of Fe 2 O 3 -rich glass at 1570 degrees C
Hartmut Schneider;
Hartmut Schneider
Deutsche Forschungsanstalt fuer Luft - und Raumfahrt, Cologne, Federal Republic of Germany
Search for other works by this author on:
Roland Pleger
Roland Pleger
Institut fuer Werkstoff-Forschung, Federal Republic of Germany
Search for other works by this author on:
Hartmut Schneider
Deutsche Forschungsanstalt fuer Luft - und Raumfahrt, Cologne, Federal Republic of Germany
Roland Pleger
Institut fuer Werkstoff-Forschung, Federal Republic of Germany
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 (1993) 5 (3): 515–521.
Article history
First Online:
02 Mar 2017
Citation
Hartmut Schneider, Roland Pleger; The reconstructive 2/1- to 3/2-mullite transformation in the presence of Fe 2 O 3 -rich glass at 1570 degrees C. European Journal of Mineralogy 1993;; 5 (3): 515–521. doi:
Download citation file:
You could not be signed in. Please check your email address / username and password and try again.
Index Terms/Descriptors
Citing articles via
Related Articles
New mineral names
American Mineralogist
Occurrence of Fe 3+ and formation process of precipitates within oxidized olivine phenocrysts in basalt lava from Kuroshima volcano, Goto islands, Nagasaki, Japan
Mineralogical Magazine
The transformation of andalusite to mullite and silica: Part I. Transformation mechanism in [001] A direction
American Mineralogist
Electron Probe Microanalysis of Trace Sulfur in Basaltic Glasses and Silicate Minerals
American Mineralogist
Related Book Content
Peridotite xenoliths from Ethiopia: Inferences about mantle processes from plume to rift settings
Volcanism and Evolution of the African Lithosphere
Geochemical and Nd isotopic constraints on the origin of uppermost Silurian rhyolitic rocks in the northern Appalachians (northern New Brunswick): Tectonic implications
New Developments in the Appalachian-Caledonian-Variscan Orogen
Phase transitions of minerals in the transition zone and upper part of the lower mantle
Advances in High-Pressure Mineralogy
The growth of the central Andes, 22°S–26°S
Geodynamics of a Cordilleran Orogenic System: The Central Andes of Argentina and Northern Chile