Skip Nav Destination
Article navigation
Other|
June 01, 1993
High-pressure stability of carbonates; quenching of calcite-II, high-pressure polymorph of CaCO 3
Claudine Biellmann;
Claudine Biellmann
Universite de Rennes I, Laboratoire de Mineralogie physique, Geosciences Rennes (CNRS), Rennes Cedex, France
Search for other works by this author on:
Claudine Biellmann
Universite de Rennes I, Laboratoire de Mineralogie physique, Geosciences Rennes (CNRS), Rennes Cedex, France
Francois Guyot
Philippe Gillet
Bruno Reynard
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): 503–510.
Article history
First Online:
02 Mar 2017
Citation
Claudine Biellmann, Francois Guyot, Philippe Gillet, Bruno Reynard; High-pressure stability of carbonates; quenching of calcite-II, high-pressure polymorph of CaCO 3. European Journal of Mineralogy 1993;; 5 (3): 503–510. 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
First evidence of CaCO 3 -III and CaCO 3 -IIIb high-pressure polymorphs of calcite: Authigenically formed in near surface sediments
American Mineralogist
Phase relations of CaCO 3 at high pressure and high temperature
American Mineralogist
Melting relations in the system CaCO 3 -MgCO 3 at 6 GPa
American Mineralogist
Related Book Content
Discovery of post-perovskite phase transition and implications for the nature of the D″ layer of the mantle
Advances in High-Pressure Mineralogy
Impact melting in sedimentary target rocks: An assessment
The Sedimentary Record of Meteorite Impacts
Relative shock effects in mixed powders of calcite, gypsum, and quartz: A calibration scheme from shock experiments
Large Meteorite Impacts and Planetary Evolution IV
Melting of ice VII and new high-pressure, high-temperature amorphous ice
Advances in High-Pressure Mineralogy