Reversed determination of the reaction: Phlogopite + quartz = enstatite + potassium feldspar + H2O in the ranges 750-875 °C and 2-12 kbar at low H2O activity with concentrated KCl solutions

American Mineralogist

Volumn 83, Issue 3-4, 1998, Pages 193-204

  Aranovich, L Y ^a   Newton, R C ^a  

^a UNIVERSITY OF CHICAGO   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

BIOTITE; CONCENTRATION (PROCESS); FELDSPAR; FREE ENERGY; IGNEOUS ROCKS; MAGNESIUM COMPOUNDS; METAMORPHIC ROCKS; MICA; MINERALOGY; POTASSIUM; POTASSIUM COMPOUNDS; QUARTZ; SILICATES; SILICON; TRANSPORT PROPERTIES;

CONCENTRATED BRINES; EXPERIMENTAL CONDITIONS; FEASIBLE ALTERNATIVES; HIGH-GRADE METAMORPHIC ROCKS; MELTING OF THE CRUSTS; METAMORPHIC CONDITIONS; METAMORPHIC PROCESS; MODERATE CONCENTRATION;

CHLORINE COMPOUNDS;

ENSTATITE; EXPERIMENTAL MINERALOGY; PHLOGOPITE; POTASSIUM FELDSPAR; QUARTZ;

EID: 0031867999     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am-1998-3-401     Document Type: Article

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