Dislocation-accommodated grain boundary sliding as the major deformation mechanism of olivine in the Earth's upper mantle

Published 2015 View Full Article

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Title
Dislocation-accommodated grain boundary sliding as the major deformation mechanism of olivine in the Earth's upper mantle
Authors
Keywords
-
Journal
Science Advances
Volume 1, Issue 9, Pages e1500360-e1500360
Publisher
American Association for the Advancement of Science (AAAS)
Online
2015-10-03
DOI
10.1126/sciadv.1500360

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