Structural evolution of a 2M1 phengite mica up to 11 GPa: An in situ single-crystal X-ray diffraction study

Physics and Chemistry of Minerals

Volumn 37, Issue 8, 2010, Pages 581-591

  Diego Gatta, G ^a,b   Rotiroti, Nicola ^a,b   Lotti, Paolo ^a   Pavese, Alessandro ^a,b   Curetti, Nadia ^c  

^a UNIVERSITY OF MILAN   (Italy)

^b CNR Consiglio Nazionale delle Ricerche   (Italy)

^c UNIVERSITY OF TURIN   (Italy)

Author keywords

Compressibility; High pressure; Mica; Phengite; Single crystal X ray diffraction

Indexed keywords

ANISOTROPIC COMPRESSION; ANISOTROPIC RESPONSE; BIRCH-MURNAGHAN EQUATION OF STATE; BULK MODULUS; COMPRESSIONAL; COOPERATIVE ROTATION; CRYSTALLINITIES; DEFORMATION MECHANISM; DIAMOND-ANVIL CELL; ELASTIC ANISOTROPY; ELASTIC BEHAVIOUR; FUNCTION OF PRESSURE; HIGH-PRESSURE; HYDROSTATIC CONDITIONS; IN-SITU; MONOTONIC DECREASE; NEGATIVE CORRELATION; NEGATIVE SLOPE; PHENGITE; ROTATION PARAMETERS; SECOND ORDERS; SINGLE CRYSTAL X-RAY DIFFRACTION; SINGLE-CRYSTAL STRUCTURE; SIX-MEMBERED RINGS; SPACE GROUPS; STRUCTURAL EVOLUTION; STRUCTURE REFINEMENTS; SYNCHROTRON X RAY POWDER DIFFRACTION; TETRAHEDRAL SHEETS; THIRD-ORDER;

ANISOTROPY; BIOLOGY; COMPRESSIBILITY; DEFORMATION; DIFFRACTION; EQUATIONS OF STATE; GEOMETRY; HIGH PRESSURE ENGINEERING; MICA; ROTATION; SILICATE MINERALS; SINGLE CRYSTALS; SODIUM; X RAY DIFFRACTION; X RAY POWDER DIFFRACTION; X RAYS;

CRYSTAL STRUCTURE;

COMPRESSIBILITY; CRYSTAL STRUCTURE; DEFORMATION MECHANISM; DIAMOND ANVIL CELL; EXPERIMENTAL MINERALOGY; HIGH PRESSURE; PHENGITE; X-RAY DIFFRACTION;

SESIA;

EID: 77956172062     PISSN: 03421791     EISSN: 14322021     Source Type: Journal    
DOI: 10.1007/s00269-010-0359-2     Document Type: Article

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