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; Juergen Reinhardt; Bruno Goffe; Laurent Jolivet; Christophe Brunet

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Other| 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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Juergen Reinhardt;

Juergen Reinhardt

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Bruno Goffe;

Bruno Goffe

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Laurent Jolivet;

Laurent Jolivet

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Christophe Brunet

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Author and Article Information

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

European Journal of Mineralogy (1997) 9 (4): 859–873.

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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

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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

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