Magma Dynamics with the Enthalpy Method: Benchmark Solutions and Magmatic Focusing at Mid-ocean Ridges
By Richard F. Katz. 2008
173 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/1a2dfb47f23aac4b3161a85ecd9e1a8457f108ee
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In Geophysics
Citations in the corpus
- Mechanisms for the generation of plate tectonics by two-phase grain-damage and pinning (2012, result): “Conservation of momentum for creeping two-phase flow has been dealt with extensively in previous studies (McKenzie, 1984, 1985, 1987; McKenzie and Holness, 2000; Spiegelman, 1993a,b,c; Bercovici et al., 2001a; Bercovici and Ricard, 2003; Katz, 2008).”
- Numerical modelling of magma dynamics coupled to tectonic deformation of lithosphere and crust (2013, background): “…magma dynamics have been concerned with the mechanical aspects of porous flow, some studies have coupled the dynamics of melt transport and host rock compaction with models of conservation of energy and composition (Richard et al. 2007; Šrámek et al. 2007; Katz 2008; Dufek & Bachmann 2010).”
- Melt Segregation in Deep Crustal Hot Zones: a Mechanism for Chemical Differentiation, Crustal Assimilation and the Formation of Evolved Magmas (2012, background): “(2003), except that we solve for enthalpy, rather than temperature, in the energy conservation equation (Katz, 2008).”
- The geodynamic equation of state: What and how (2009, methodology): “The s–P–m formulation is essentially the enthalpy method of chemical engineering [Oezisik, 1993], which has been applied to geodynamic models with parameterized phase equilibria [Katz, 2008].”
- The Role of Volatiles in Reactive Melt Transport in the Asthenosphere (2015, unknown): “Melt viscosity l, however, has been treated as a constant in previous studies (e.g. Spiegelman et al., 2001; Katz, 2008; Hewitt, 2010; Liang et al., 2010; Weatherley & Katz, 2012).”
- Organized melt, seismic anisotropy, and plate boundary lubrication (2010, background): “Interactions of these processes have been modeled extensively in various combinations [e.g., Phipps Morgan, 1997; Braun et al., 2000; Katz, 2008], but coupling and feedbacks between melting, melt distribution, viscosity (with segregated melt), mantle flow and thermal structure have not yet been…”