Slab weakening during the olivine to ringwoodite transition in the mantle
- 1 February 2020
- journal article
- research article
- Published by Springer Science and Business Media LLC in Nature Geoscience
- Vol. 13 (2), 170-+
- https://doi.org/10.1038/s41561-019-0523-3
Abstract
No abstract availableFunding Information
- National Science Foundation
This publication has 38 references indexed in Scilit:
- Shear deformation of dry polycrystalline olivine under deep upper mantle conditions using a rotational Drickamer apparatus (RDA)Physics of the Earth and Planetary Interiors, 2009
- Plastic deformation of wadsleyite and olivine at high-pressure and high-temperature using a rotational Drickamer apparatus (RDA)Physics of the Earth and Planetary Interiors, 2008
- Water controls the fields of metastable olivine in cold subducting slabsGeophysical Research Letters, 2005
- Thermal equation of state of (Mg0.91Fe0.09)2SiO4 ringwooditePhysics of the Earth and Planetary Interiors, 2004
- Single‐crystal elasticity of γ‐(Mg0.91Fe0.09(2SiO4 to high pressures and to high temperaturesGeophysical Research Letters, 2001
- Phase transition buoyancy contributions to stresses in subducting lithosphereGeophysical Research Letters, 1996
- Kinetics of the olivine-spinel transformation in subducting lithosphere: experimental constraints and implications for deep slab processesPhysics of the Earth and Planetary Interiors, 1994
- Flow laws for rocks containing two non-linear viscous phases: A phenomenological approachJournal of Structural Geology, 1994
- Current plate velocities relative to the hotspots incorporating the NUVEL‐1 global plate motion modelGeophysical Research Letters, 1990
- Kinetics of high-pressure phase transformations: Implications to the evolution of the olivine → spinel transition in the downgoing lithosphere and its consequences on the dynamics of the mantleTectonophysics, 1976