Causes and consequences of flow organization during melt transport: The reaction infiltration instability in compactible media

By Marc Spiegelman, P. Kelemen, E. Aharonov. 2001

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In Geophysics

Citations in the corpus

Stress‐driven melt segregation in partially molten rocks (2003, background): “This process tends to produce runaway instabilities which take the form of channels organized into a coalescing network [e.g., Spiegelman et al., 2001].”
The Role of Volatiles in Reactive Melt Transport in the Asthenosphere (2015, methodology): “Studies that followed have applied simple reactive flow models to magma transport in a mantle column with increasing solubility of a fertile component with decreasing pressure (Aharonov et al., 1995; Spiegelman et al., 2001; Liang et al., 2010; Hesse et al., 2011).”
Wormhole formation in dissolving fractures (2009, background): “Spontaneous channeling of a reactive front has been shown to be important for a number of geophysical processes, such as diagenesis [Chen et al., 1990; Boudreau, 1996], melt migration [Daines and Kohlstedt, 1994; Aharonov et al., 1995; Kelemen et al., 1995; Spiegelman and Kelemen, 1995 ], terra ros”
TIDALLY HEATED TERRESTRIAL EXOPLANETS: VISCOELASTIC RESPONSE MODELS (2009, background): “For the most vigorous exoworlds, the assumption of convective heat transfer gives way to a regime dominated by advective heat transport (Spiegelman et al. 2001).”
Numerical modelling of magma dynamics coupled to tectonic deformation of lithosphere and crust (2013, background): “…(Stevenson 1989; Richardson 1998; Katz et al. 2006), the reactive melt band instability (Aharonov et al. 1995, 1997; Kelemen et al. 1997; Spiegelman et al. 2001; Weatherley & Katz 2012) and the decompaction channeling instability (Connolly & Podladchikov 2007), or with (iv) the…”
Vertically extensive and unstable magmatic systems: A unified view of igneous processes (2017, unknown): “Mushes are multiphase systems in which buoyant melt (and sometimes fluids) are distributed within a deformable crystalline matrix; the dynamics of such systems are characterised by compaction-driven segregation of melts and fluids from the crystalline matrix ( 22-24 , 105 ).”
Viscous constitutive relations of solid-liquid composites in terms of grain boundary contiguity: 1. Grain boundary diffusion control model (2009, background): “Several mechanisms for channel formation have been proposed including the reaction infiltration instability [e.g., Spiegelman et al., 2001 ] and shear-induced melt segregation [e.g., Stevenson, 1989; Spiegelman, 2003; Katz et al., 2006].”
Fate of Pyroxenite-derived Melts in the Peridotitic Mantle: Thermodynamic and Experimental Constraints (2012, methodology): “The following models have been proposed to explain melt focusing: (1) formation of self-organized dissolution channels by reactive infiltration instability (e.g. Daines & Kohlstedt, 1994; Spiegelman et al., 2001); (2) dike formation by hydraulic fracturing (e.”
Magma Dynamics with the Enthalpy Method: Benchmark Solutions and Magmatic Focusing at Mid-ocean Ridges (2008, background): “The inclusion of pressure gradients caused by compaction allows for localization of melt as a result of reactive (e.g. Aharonov et al., 1995; Spiegelman et al., 2001) and mechanical (e.”