Deformation of Earth Materials: Contents

By S. Karato. 2008

286 citations recorded by the source corpus.

Subfields: Earth-Surface Processes, Geophysics, Mechanics of Materials

View Paper: https://www.semanticscholar.org/paper/c6147bde5cdd3e8ef9c253930092dcde84e24609

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Earth-Surface Processes

1. Antoine Rozel
2. D. Bercovici
3. Y. Ricard
4. M. Long
5. Jun Korenaga
6. P. Silver
7. Sylvain Barbot
8. Y. Fialko

In Geophysics

1. S. Karato
2. Jun Korenaga
3. Y. Ricard
4. M. Long
5. D. Bercovici
6. I. Katayama
7. H. Jung
8. P. Silver

In Mechanics of Materials

1. D. Bercovici
2. Y. Ricard
3. Antoine Rozel
4. S. Karato
5. M. Long
6. Jun Korenaga
7. P. Silver
8. Sylvain Barbot

Citations in the corpus

• Geodynamic Significance of Seismic Anisotropy of the Upper Mantle: New Insights from Laboratory Studies (2008, background): “A generic form for a flow law is (e.g., Karato 2008) ε̇ = A · ( 1 + B · f rH2O ) · σ n · exp ( − H ∗ RT ( 1 − ( σ σP )q )s ) , (4) where A is a pre-exponential factor, B is a constant, σP is the Peierls stress, and q and r are nondimensional constants that depend on the process of dislocation glide.”
• GEODYNAMICS AND RATE OF VOLCANISM ON MASSIVE EARTH-LIKE PLANETS (2008, background): “The degree to which the mantle cools over geological time depends on the activation energy for deformation of mantle rock, which is known only imprecisely (Karato 2008).”
• A new analysis of experimental data on olivine rheology (2008, background): “Citation: Korenaga, J., and S.-I. Karato (2008), A new analysis of experimental data on olivine rheology, J. Geophys.”
• 3‐D multiobservable probabilistic inversion for the compositional and thermal structure of the lithosphere and upper mantle. I: a priori petrological information and geophysical observables (2013, background): “Consequently, considering typical water contents in mantle rocks (<200– 400 ppm), melt extractions of only <10% can effectively “dry out” the residue, significantly increasing its electrical resistivity and viscosity relative to its hydrated counterpart [e.g., Karato, 2008; Jones et al., 2012].”
• Shear Wave Splitting and Mantle Anisotropy: Measurements, Interpretations, and New Directions (2009, background): “Overall, however, there is very little experimental data on LPO development in transition zone materials (Karato 2008).”
• A thermodynamically self-consistent damage equation for grain size evolution during dynamic recrystallization (2011, methodology): “Three reversible terms can be considered: the macroscopic elastic energy, the energy of dislocations (Karato 2008) and the surface energy of grains, γ (in J m−2).”
• A unified continuum representation of post-seismic relaxation mechanisms: semi-analytic models of afterslip, poroelastic rebound and viscoelastic flow (2010, background): “The ductile flow is not limited by a yield surface and for a constant stress condition the effective viscosity η increases exponentially with decreasing temperature (e.g. Karato 2008).”
• The viscosity of Earth's lower mantle inferred from sinking speed of subducted lithosphere (2012, background): “For the lower mantle, particularly, only few constraints result from elaborate high-pressure experiments (Karato, 2008) and a variety of viscosity depth profiles result from joint inversion of the geoid and postglacial rebound data (Forte and Mitrovica, 1996; Kaufmann and Lambeck, 2000; Mitrovica…”