Energetics of a two-phase model of lithospheric damage, shear localization and plate-boundary formation

By D. Bercovici, Y. Ricard. 2003

154 citations recorded by the source corpus.

Subfields: Geophysics, Mechanics of Materials

View Paper: https://www.semanticscholar.org/paper/5bbea238c5e14cc73783481810f93b1691dd3893

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In Geophysics

1. Tobias Keller
2. Richard F. Katz
3. Y. Ricard
4. D. Bercovici
5. B. Kaus
6. D. May
7. Marc Spiegelman
8. Cian R. Wilson

In Mechanics of Materials

1. Richard F. Katz
2. Tobias Keller
3. B. Kaus
4. D. Bercovici
5. D. May
6. Y. Ricard
7. Cian R. Wilson

Citations in the corpus

• Fluid flow in subduction zones: The role of solid rheology and compaction pressure (2014, background): “1) as approximations of the general equations for fluid flow in viscously deformable porous media (McKenzie, 1984; Scott and Stevenson, 1984; Scott and Stevenson, 1986; Bercovici and Ricard, 2003; Simpson et al., 2010a; Simpson et al., 2010b).”
• The generation of plate tectonics from mantle convection (2003, background): “9), in addition to broadly distributed damage when the entire system essentially shatters [65,66].”
• Numerical modelling of magma dynamics coupled to tectonic deformation of lithosphere and crust (2013, methodology): “The physics of two-phase flow in the context of geodynamics have been derived in various studies (e.g. Sleep 1974; McKenzie 1984; Fowler 1985; Scott & Stevenson 1986; Spiegelman 1993a,b; Bercovici et al. 2001a; Bercovici & Ricard 2003).”
• Magma Dynamics with the Enthalpy Method: Benchmark Solutions and Magmatic Focusing at Mid-ocean Ridges (2008, background): “However it was shown by Bercovici & Ricard (2003) that in the case relevant to magma dynamics of a fluid with viscosity that is much smaller that the matrix viscosity (and neglecting surface tension and damage), the general equations reduce to the set derived by McKenzie (1984).”
• Mechanisms for the generation of plate tectonics by two-phase grain-damage and pinning (2012, methodology): “Following the same arguments for determining the interface pressure P∗ as in Bercovici et al. (2001a) and Bercovici and Ricard (2003), and defining an effective internal pressure Πi = Pi + γiKi, equation (D.1) becomes 0 = − ∇(φiΠi) + ∇ · (φiτi) + ρiφig + c∆vi + (∑ j (1 − ω j)Π j ) ∇φi + ωi∇(γIα)…”