Grain misorientations in partially molten olivine aggregates: an electron backscatter diffraction study
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Faul, Ulrich; Fitz Gerald, John
Description
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.
| Collections | ANU Research Publications |
|---|---|
| Date published: | 1999 |
| Type: | Journal article |
| URI: | http://hdl.handle.net/1885/93913 |
| Source: | Physics and Chemistry of Minerals |
| DOI: | 10.1007/s002690050176 |
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| File | Description | Size | Format | Image |
|---|---|---|---|---|
| 01_Faul_Grain_misorientations_in_1999.pdf | 1.08 MB | Adobe PDF | Request a copy |
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