1981American MineralogistRequires access

High-pressure structural study of diopside

L. Levien, Charles T. Prewitt

Open publisher page 252 citations

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.

About this research paper

What this paper is about

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.

Why it matters

OpenAlex reports 252 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available 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.

Key concepts: Diopside, Silicate, Mineralogy, Geology, High pressure, Crystallography, Materials science, Thermodynamics

Related papers

Back to paper searchBrowse research topicsOriginal source
High-pressure structural study of diopside — Research Paper | ScholarLens