Synthetic hypersilicic Cl-bearing mica in the phlogopite-celadonite join: A multimethodical characterization of the missing link between di- and tri-octahedral micas at high pressures

American Mineralogist

Volumn 93, Issue 8-9, 2008, Pages 1429-1436

  Nazzareni, Sabrina ^a   Comodi, Paola ^a   Bindi, Luca ^b   Safonov, Oleg G ^c   Litvin, Yuriy A ^c   Perchuk, Leonid L ^c,d  

^a UNIVERSITY OF PERUGIA   (Italy)

^b UNIVERSITY OF FLORENCE   (Italy)

^c INSTITUTE OF EXPERIMENTAL MINERALOGY   (Russian Federation)

^d MOSCOW STATE UNIVERSITY   (Russian Federation)

Author keywords

Al celadonite; Chlorine; High pressure; Inclusions in diamonds; Kimberlites; Phlogopite; Solid solution

Indexed keywords

CHLORINE; CRYSTAL STRUCTURE; DIAMOND DEPOSITS; POTASSIUM COMPOUNDS; SILICON; SINGLE CRYSTALS; SOLID SOLUTIONS; SYNTHESIS (CHEMICAL); VOLCANIC ROCKS;

ALUMINOSILICATE GLASS; HIGH PRESSURE; INCLUSIONS IN DIAMOND; KIMBERLITES; NEGATIVE CORRELATION; PHLOGOPITE; SINGLE CRYSTAL X-RAY DIFFRACTION; STRUCTURE REFINEMENTS;

MICA;

CELADONITE; CRYSTAL CHEMISTRY; EXPERIMENTAL MINERALOGY; HIGH PRESSURE; PHLOGOPITE; RAMAN SPECTROSCOPY; SOLID SOLUTION; X-RAY DIFFRACTION;

MICAS;

EID: 50849143178     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am.2008.2802     Document Type: Article

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