Stress and Strain Rate Evolution During the Finite Strain Deformation of a Weak Ferropericlase Grain by Diffusion Creep: Implications for Shear Localization in the Lower Mantle-Reference-Cited by-同舟云学术

Stress and Strain Rate Evolution During the Finite Strain Deformation of a Weak Ferropericlase Grain by Diffusion Creep: Implications for Shear Localization in the Lower Mantle

Published:2021-12-30 Issue:1 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Cho H. E.¹²^ORCID,Karato Shun‐ichiro¹^ORCID

Affiliation:

1. Department of Earth and Planetary Sciences Yale University New Haven CT USA

2. School of Engineering Liberty University Lynchburg VA USA

Funder

Yale University

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JB022673

Reference52 articles.

1. Application of bound theorems for creeping solids and their application to large strain diffusional flow

2. Persistence of strong silica-enriched domains in the Earth’s lower mantle

3. The finite deformation of an inhomogeneity in two-dimensional slow viscous incompressible flow

4. Correlating mechanical data with microstructural observations in deformation experiments on synthetic two-phase aggregates

5. Pure climb creep mechanism drives flow in Earth’s lower mantle

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