Coupled flow and anisotropy in the UltraLow Velocity Zones
Author:
Funder
NSF
Publisher
Elsevier BV
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Reference41 articles.
1. Thermal and chemical evolution of the terrestrial magma ocean;Abe;Phys. Earth Planet. Inter.,1997
2. A geodynamic and mineral physics model of a solid-state ultralow-velocity zone;Bower;Earth Planet. Sci. Lett.,2011
3. 142Nd evidence for early (>4.53 Ga) global differentiation of the silicate Earth;Boyet;Science,2005
4. Crystallization of a basal magma ocean recorded by helium and neon;Coltice;Earth Planet. Sci. Lett.,2011
5. An unusually large ULVZ at the base of the mantle near Hawaii;Cottaar;Earth Planet. Sci. Lett.,2012
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1. Sensitivity of SK(K)S and ScS phases to heterogeneous anisotropy in the lowermost mantle from global wavefield simulations;Geophysical Journal International;2021-08-06
2. The morphology, evolution and seismic visibility of partial melt at the core-mantle boundary: Implications for ULVZs;Geophysical Journal International;2021-06-25
3. Modeling Ultralow Velocity Zones as a Thin Chemically Distinct Dense Layer at the Core‐Mantle Boundary;Journal of Geophysical Research: Solid Earth;2019-08
4. An investigation of seismic anisotropy in the lowermost mantle beneath Iceland;Geophysical Journal International;2019-07-11
5. Analytical solution for two-phase flow within and outside a sphere under pure shear;Journal of Fluid Mechanics;2018-06-13
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