Deformation across the mantle transition zone: A theoretical mineral physics view
Author:
Funder
Horizon 2020
European Research Council
Publisher
Elsevier BV
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Reference86 articles.
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3. Steady state and low stresses in lithospheric mantle inferred from dislocation modelling of creep in olivine;Boioli;Earth Planet. Sci. Lett.,2015
4. Modeling the creep properties of olivine by 2.5-D dislocation dynamics simulations;Boioli;Phys. Rev. B,2015
5. Pure climb creep mechanism drives flow in the Earth's lower mantle;Boioli;Sci. Adv.,2017
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1. On Dislocation Climb as an Important Deformation Mechanism for Planetary Interiors;Annual Review of Earth and Planetary Sciences;2024-07-23
2. Pressure-dependent large-scale seismic anisotropy induced by non-Newtonian mantle flow;Geophysical Journal International;2024-05-06
3. Deformation Mechanisms, Microstructures, and Seismic Anisotropy of Wadsleyite in the Earth's Transition Zone;Geochemistry, Geophysics, Geosystems;2023-11
4. Grain size reduction by plug flow in the wet oceanic upper mantle explains the asthenosphere's low seismic Q zone;Earth and Planetary Science Letters;2023-08
5. Twinning in hydrous wadsleyite: symmetry relations, origin, and consequences;American Mineralogist;2023-01-01
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