학술논문

Neutron-diffraction structure of a low-water grossular at 20 K
Document Type
Journal Article
Author
Source
Am. Mineral.; (United States); 72:7-8
Subject
58 GEOSCIENCES GARNETS
CRYSTAL STRUCTURE
CRYSTALLOGRAPHY
QUANTITATIVE CHEMICAL ANALYSIS
MINERALOGY
NEUTRON DIFFRACTION
SILICA
TEMPERATURE EFFECTS
CHALCOGENIDES
CHEMICAL ANALYSIS
COHERENT SCATTERING
DIFFRACTION
MINERALS
OXIDE MINERALS
OXIDES
OXYGEN COMPOUNDS
SCATTERING
SILICATES
SILICON COMPOUNDS
SILICON OXIDES 580300* -- Mineralogy, Petrology, & Rock Mechanics-- (-1989)
Language
English
Abstract
The crystal structure of a low-water (0.16 wt% OH) grossular has been refined at 20 K by single-crystal time-of-flight neutron-diffraction methods. Comparisons with the room-temperature structure indicate that between 298 and 20 K, the silicate tetrahedron undergoes a small rigid-body rotation that results in an increase in the y parameter of oxygen. The mechanism of thermal expansion is significantly different from that at high temperature where the tetrahedra do not rotate and changes in the structure reflect only unit-cell expansion.