High-pressure structural study of diopside
L. Levien, Charles T. Prewitt
Abstract
L. Levien, Charles T. Prewitt
Abstract
High-pressure structural studies performed on diopside at five pressures between I atm and 53 kbar show that the three polyhedra that comprise the structure, M(l), M(2), and Si, de crease irregularly in size. The polyhedral volumes of M(l) and M(2) both decrease approxi mately 5%, whereas that of Si decreases only 1%. Comparison of high-pressure structural changes of diopside and fassaite (another clinopyroxen e) shows substantial differences, with diopside showing less tetrahedral and M(l) compression and more silicate-chain kinking.
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High-pressure structural studies performed on diopside at five pressures between I atm and 53 kbar show that the three polyhedra that comprise the structure, M(l), M(2), and Si, de crease irregularly in size. The polyhedral volumes of M(l) and M(2) both decrease approxi mately 5%, whereas that of Si decreases only 1%. Comparison of high-pressure structural changes of diopside and fassaite (another clinopyroxen e) shows substantial differences, with diopside showing less tetrahedral and M(l) compression and more silicate-chain kinking.
Key concepts: Diopside, Silicate, Mineralogy, Geology, High pressure, Crystallography, Materials science, Thermodynamics