The symmetry of garnets on the pyrope (Mg3Al2Si3O12) -majorite (MgSiO3)

Geophysical Research Letters

Volumn 23, Issue 25, 1996, Pages 3799-3802

  Parise, John B ^a  

^a STONY BROOK UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ELECTRON DIFFRACTION APPARATUS; HIGH RESOLUTION TRANSMISSION ELECTRON MICROSCOPY; TRANSMISSION ELECTRON MICROSCOPY; X RAY POWDER DIFFRACTION; COMPOSITION EFFECTS; CRYSTAL SYMMETRY; ELASTIC MODULI; GARNETS; PHASE TRANSITIONS; RHEOLOGY; SYNTHESIS (CHEMICAL); THERMAL EFFECTS;

ANOMALOUS BEHAVIOR; EARTH'S MANTLE; ELASTIC SHEAR MODULUS; HIGH RESOLUTION; RHEOLOGICAL PROPERTY; STRUCTURAL PHASE TRANSITION; SYNCHROTRON X RAY POWDER DIFFRACTION; TRANSITION ZONES;

GARNETS; GEOPHYSICS;

EARTH MANTLE TRANSITION ZONE; MAJORITE; PYROPE; SYNCHROTRON X RAY POWDER DIFFRACTION ANALYSIS; UNIAXIAL SPLIT SPHERE APPARATUS;

GARNET; MAJORITE; P/T CONDITIONS; PHASE TRANSITION; PYROPE;

EID: 0030419075     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/96GL03613     Document Type: Article

References (2)

1. 12 at high pressures and temperatures, Phys. Earth Planet. Interiors, 15, 90-106, 1977.
2. Ando, J., J. Chen, D. J. Weidner, Y. Wu and Y. Wang, In-situ measurement of rheology in silicate garnets at high pressure and temperature, Fall 1996 AGU meeting, EOS, in press, 1996.