Substitution mechanisms and implications for the estimate of water fugacity for Ti-rich phlogopite from Mt. Vulture, Potenza, Italy

American Mineralogist

Volumn 96, Issue 8-9, 2011, Pages 1381-1391

  Lacalamita, M ^a   Schingaro, E ^a   Scordari, F ^a   Ventruti, G ^a   Fabbrizio, A ^b   Pedrazzi, G ^c  

^a UNIVERSITY OF BARI   (Italy)

^b UNIVERSITY OF INNSBRUCK   (Austria)

^c UNIVERSITY OF PARMA   (Italy)

Author keywords

Crystal chemistry; FTIR spectroscopy; Geohygrometer; M ; Ssbauer spectroscopy; Ti phlogopite

Indexed keywords

CRYSTAL CHEMISTRY; ELECTRON PROBE MICROANALYSIS; FELDSPAR; FOURIER TRANSFORM INFRARED SPECTROSCOPY; MAGNETITE; MICA; MOLYBDENUM METALLOGRAPHY; SINGLE CRYSTALS;

CRYSTAL-CHEMICAL FEATURES; FTIR SPECTROSCOPY; GEOHYGROMETER; LOCAL CONFIGURATIONS; SINGLE CRYSTAL X-RAY DIFFRACTION; SSBAUER SPECTROSCOPIES; STRUCTURE REFINEMENTS; SUBSTITUTION MECHANISMS;

TITANIUM METALLOGRAPHY;

CRYSTAL CHEMISTRY; ELECTRON PROBE ANALYSIS; FTIR SPECTROSCOPY; FUGACITY; HOST ROCK; IGNIMBRITE; MAGNETITE; PHLOGOPITE; SANIDINE; STOICHIOMETRY; TITANIUM; X-RAY DIFFRACTION;

BASILICATA; ITALY; MOUNT VULTURE; POTENZA;

EID: 80053282322     PISSN: 0003004X     EISSN: 19453027     Source Type: Journal    
DOI: 10.2138/am.2011.3772     Document Type: Article

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