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August 01, 1997
Ferro- and magnesiocarpholite from the Monte Argentario (Italy); first evidence for high-pressure metamorphism of the metasedimentary Verrucano sequence, and significance for P-T path reconstruction
Thomas Theye;
Thomas Theye
Universitaet Stuttgart, Institut fuer Mineralogie und Kristallchemie, Stuttgart, Federal Republic of Germany
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Thomas Theye
Universitaet Stuttgart, Institut fuer Mineralogie und Kristallchemie, Stuttgart, Federal Republic of Germany
Juergen Reinhardt
Bruno Goffe
Laurent Jolivet
Christophe Brunet
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 (1997) 9 (4): 859–873.
Article history
First Online:
02 Mar 2017
Citation
Thomas Theye, Juergen Reinhardt, Bruno Goffe, Laurent Jolivet, Christophe Brunet; Ferro- and magnesiocarpholite from the Monte Argentario (Italy); first evidence for high-pressure metamorphism of the metasedimentary Verrucano sequence, and significance for P-T path reconstruction. European Journal of Mineralogy 1997;; 9 (4): 859–873. doi:
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Index Terms/Descriptors
- Apennines
- chain silicates
- Europe
- ferrocarpholite
- high pressure
- high-grade metamorphism
- Italy
- metamorphic rocks
- metamorphism
- metapelite
- metasedimentary rocks
- Northern Apennines
- P-T conditions
- pressure
- silicates
- Southern Europe
- thermodynamic properties
- Verrucano Formation
- Monte Argentario
- magnesiocarpholite
Latitude & Longitude
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