Skip navigation
Skip navigation

Grain misorientations in partially molten olivine aggregates: an electron backscatter diffraction study

Faul, Ulrich; Fitz Gerald, John


In polycrystalline aggregates of olivine with mean grain sizes above 35 μm plus a low basaltic melt fraction, both wetted and melt-free grain boundaries are observed after equilibration times at high pressures and temperatures of between 15 and 25 days.

CollectionsANU Research Publications
Date published: 1999
Type: Journal article
Source: Physics and Chemistry of Minerals
DOI: 10.1007/s002690050176


File Description SizeFormat Image
01_Faul_Grain_misorientations_in_1999.pdf1.08 MBAdobe PDF    Request a copy

Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.

Updated:  17 November 2022/ Responsible Officer:  University Librarian/ Page Contact:  Library Systems & Web Coordinator