To use all functions of this page, please activate cookies in your browser.
With an accout for my.chemeurope.com you can always see everything at a glance – and you can configure your own website and individual newsletter.
- My watch list
- My saved searches
- My saved topics
- My newsletter
Continuous sub-grain rotation type dynamic recrystallization
In Metallurgy, Materials Science and Structural geology continuous sub-grain rotation type dynamic recrystallization is recognized as an important mechanism for dynamic recrystallisation. It involves the rotation of initially low-angle sub-grain boundaries until the mismatch between the crystal lattices across the boundary is sufficient for them to be regarded as grain boundaries. This mechanism has been recognized in many minerals, including; quartz, calcite, olivine, pyroxenes, micas, feldspars, halite and garnets, and in metals; various magnesium, aluminium and nickel alloys.
|This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Continuous_sub-grain_rotation_type_dynamic_recrystallization". A list of authors is available in Wikipedia.|