Deformation of Earth Materials : an Introduction to the Rheology of Solid Earth

By 唐戸 俊一郎. 2008

334 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/0ee4cbd7eb71e06048d98d0bab23ea967c67512d

How researchers see this paper

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

1. Jun Korenaga
2. D. Bercovici
3. S. Karato
4. Y. Ricard
5. Antoine Rozel
6. D. Sasselov
7. R. O’Connell
8. A. Berg

Citations in the corpus

• 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…”
• TIDALLY HEATED TERRESTRIAL EXOPLANETS: VISCOELASTIC RESPONSE MODELS (2009, background): “…dissipation measurements from Earth’s Chandler wobble, tides and free oscillations, summarized in Karato & Spetzler (1990) show Q values which change gradually with frequency, and are modeled well by empirical power laws of the form Q ∼ ωαQ (αQ = 0.1 to 0.4) (Karato 2007; Efroimsky & Lainey 2007).”
• A new analysis of experimental data on olivine rheology (2008, methodology): “In comparing results from experimental data for different deformation geometry, we make an assumption of isotropic plasticity and use the Levy-von Mises formula [e.g., Karato, 2007, Chap.”
• 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).”
• Tidal torques: a critical review of some techniques (2008, unknown): “∆tlmpq = ω ∗ lmpq ∆tlmpq = ±χlmpq ∆tlmpq , (24) the tidal harmonic ω lmpq being introduced as ω lmpq ≡ (l − 2p) ω̇ + (l − 2p + q) Ṁ + m (Ω̇ − θ̇) , (25) the positively-defined physical frequency χlmpq ≡ |ω lmpq | = | (l − 2p) ω̇ + (l − 2p + q)Ṁ + m (Ω̇ − θ̇) | (26) being the actual physical lmpq tid”
• Water distribution across the mantle transition zone and its implications for global material circulation (2011, unknown): “These values are less than the influence of temperature (a temperature variation of 100 K will cause the velocity variation of ~0.7%, Karato, 2008a).”
• On the origin of the asthenosphere (2012, background): “Also there is exceptionally strong radial anisotropy in the asthenosphere of the central Pacific (Ekström and Dziewonski, 1998; Karato, 2008b), that affects the global model of radial anisotropy (Nettles and Dziewonski, 2008).”
• Rheology of the Earth's mantle: A historical review (2010, methodology): “In most cases, seismic anisotropy is caused by the lattice-preferred orientation of elastically anisotropic minerals (e.g., Chapter 21 of Karato, 2008).”