Competing Deformation Mechanisms in Periclase: Implications for Lower Mantle Anisotropy
Seismic anisotropy is observed above the core-mantle boundary in regions of slab subduction and near the margins of Large Low Shear Velocity Provinces (LLSVPs). Ferropericlase is believed to be the second most abundant phase in the lower mantle. As it is rheologically weak, it may be a dominant sour...
Main Authors: | Feng Lin, Samantha Couper, Mike Jugle, Lowell Miyagi |
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Format: | Article |
Language: | English |
Published: |
MDPI AG
2019-10-01
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Series: | Minerals |
Subjects: | |
Online Access: | https://www.mdpi.com/2075-163X/9/11/650 |
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