Structural evolution, magnetic transitions, and the gruneisen constants of the antimonites MeSb2O4
Author:
Affiliation:
1. a Laboratoire Chimie Physique du Solide U.A. 453 CNRS, 92295 , Chatenay-Malabry Cedex et Université Paris XIII , 93430, Villetaneuse , France
Publisher
Informa UK Limited
Subject
General Materials Science,Instrumentation
Link
https://www.tandfonline.com/doi/pdf/10.1080/01411598908208087
Reference10 articles.
1. Thermodynamic studies on antimonites MSb2O4 (M = Ni,Fe) in the temperature range 10 to 300 K
2. Evolution structure entre 2 et 300 K de l'oxyde MnSb2O4: Proprie´te´se´lastiques et magne´tiques anisotropes
3. Composes isomorphes MeX2O4E2
4. Structures isomorphes MeX2O4—Evolution structurale entre 2 K et 300 K de l'antimonite FeSb2O4: Elasticité et ordre magnétique anisotropes
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1. Advances in data reduction of high-pressure x-ray powder diffraction data from two-dimensional detectors: a case study of schafarzikite (FeSb2O4);Journal of Physics: Condensed Matter;2006-06-09
2. Bulk moduli and high-pressure crystal structures of minium, Pb3O4, determined by X-ray powder diffraction;American Mineralogist;2003-07
3. Anisotropic thermal expansion and Grüneisen coefficients of the bismuth cuprate 2-2-1-2;Materials Letters;1994-01
4. Structural evolution, thermal expansion anomaly and the Grüneisen constants of the superconductor YBa2Cu3O7;Physica C: Superconductivity;1990-03
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