The phase boundary between α- and β-Mg2SiO 4 determined by in situ x-ray observation

Science

Volumn 265, Issue 5176, 1994, Pages 1202-1203

  Morishima, H ^a   Kato, T ^a   Suto, M ^a   Ohtani, E ^a   Urakawa, S ^b   Utsumi, W ^c   Shimomura, O ^d   Kikegawa, T ^d  

^a TOHOKU UNIVERSITY   (Japan)

^b OKAYAMA UNIVERSITY   (Japan)

^c UNIVERSITY OF TOKYO   (Japan)

^d HIGH ENERGY ACCELERATOR RESEARCH ORGANIZATION KEK   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

OLIVINE; P/T CONDITIONS; PHASE RELATIONS;

HIGH PRESSURE EFFECTS; MATHEMATICAL MODELS; PHASE DIAGRAMS; PHASE TRANSITIONS; SILICATE MINERALS; SYNCHROTRON RADIATION; THERMODYNAMICS; X RAY ANALYSIS;

EARTH'S UPPER MANTLE MINERALS; HIGH PRESSURE DIAMOND ANVILS; OLIVINE-TO-SPINEL PHASE TRANSITIONS; PHASE TRANSITION BOUNDARIES; PRESSURE INDUCED PHASE TRANSITIONS; SYNCHROTRON RADIATION X RAY SOURCES; X RAY DIFFRACTION ANALYSIS;

GEOPHYSICS;

EID: 0028486376     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.265.5176.1202     Document Type: Article

References (14)