The high-pressure monazite-to-scheelite transformation in CaSeO 4

Mineralogical Magazine

Volumn 76, Issue 4, 2012, Pages 913-923

  Crichton, W A ^a,b   Merlini, M ^c   Muller H ^a   Chantel, J ^a   Hanfland, M ^a  

^a EUROPEAN SYNCHROTRON RADIATION FACILITY   (France)

^b UNIVERSITY COLLEGE LONDON   (United Kingdom)

^c UNIVERSITY OF MILAN   (Italy)

Author keywords

high pressure; monazite; powder diffraction; scheelite; synchrotron

Indexed keywords

AMBIENT CONDITIONS; FIRST ORDER TRANSITIONS; HIGH PRESSURE; HIGH-PRESSURE AND TEMPERATURES; POWDER DIFFRACTION; RECOVERED MATERIALS; SCHEELITE; SCHEELITE STRUCTURE; SPACE GROUPS; SYNCHROTRON X RAY POWDER DIFFRACTION; TRANSITION SEQUENCES; UNIT CELLS; VOLUME CHANGE;

DIFFRACTION; MONAZITE; PHOSPHATE MINERALS; SELENIUM COMPOUNDS; SYNCHROTRONS; TRANSITION METAL COMPOUNDS; X RAY POWDER DIFFRACTION;

TUNGSTATE MINERALS;

ARSENATE; EXPERIMENTAL MINERALOGY; HIGH PRESSURE; HIGH TEMPERATURE; MONAZITE; ORTHOPHOSPHATE; SCHEELITE; SELENATE; SULFATE GROUP; TRANSFORMATION; VANADATE GROUP; X-RAY DIFFRACTION;

EID: 84865027780     PISSN: 0026461X     EISSN: 14718022     Source Type: Journal    
DOI: 10.1180/minmag.2012.076.4.08     Document Type: Article

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