High-pressure/low-temperature metamorphism of the Ko-hegy Gneiss, Sopron (W-Hungary); phengite barometry and fluid inclusions

Kalman Torok

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Other| October 01, 1996

High-pressure/low-temperature metamorphism of the Ko-hegy Gneiss, Sopron (W-Hungary); phengite barometry and fluid inclusions

Kalman Torok

Eotvos Lorand Univ., Budapest, Hungary

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Author and Article Information

Kalman Torok

Eotvos Lorand Univ., Budapest, Hungary

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 (1996) 8 (5): 917–925.

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High-pressure/low-temperature metamorphism of the Ko-hegy Gneiss, Sopron (W-Hungary); phengite barometry and fluid inclusions

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