Structures related to those of spinel and theβ-phase, and a possible mechanism for the transformation olivine ↔ spinel
- 1 January 1982
- journal article
- Published by Walter de Gruyter GmbH in Zeitschrift für Kristallographie
- Vol. 160 (1-2), 53-62
- https://doi.org/10.1524/zkri.1982.160.1-2.53
Abstract
No abstract availableThis publication has 10 references indexed in Scilit:
- Why olivine transforms to spinel at high pressureNature, 1981
- Cross-slip characterization in spinel MgO.1·8 A12O3deformed at high temperaturesPhilosophical Magazine A, 1981
- Structure of nickel aluminosilicate (phase V): a high-pressure phase related to spinelActa Crystallographica Section B: Structural Science, Crystal Engineering and Materials, 1981
- Structure of nickel aluminosilicate (phase IV): a high-pressure phase related to spinelActa Crystallographica Section B: Structural Science, Crystal Engineering and Materials, 1981
- The (twin) composition plane as an extended defect and structure-building entity in crystalsProgress in Solid State Chemistry, 1979
- Nickel aluminosilicate, phase IIActa Crystallographica Section B: Structural Science, Crystal Engineering and Materials, 1975
- Nickel aluminosilicate, phase IActa Crystallographica Section B: Structural Science, Crystal Engineering and Materials, 1975
- New orthorhombic phases on the join NiAl2O4 (spinel analog)-Ni2SiO4 (olivine analog): Stability and implications to mantle mineralogyContributions to Mineralogy and Petrology, 1974
- Modified Spinel, Beta-Manganous Orthogermanate: Stability and Crystal StructureScience, 1969
- Synthesis of Mg2SiO4-Fe2SiO4 spinel solid solutionsEarth and Planetary Science Letters, 1966