Stress‐driven melt segregation in partially molten rocks
By Benjamin K. Holtzman, N. Groebner, M. Zimmerman, S. Ginsberg, D. Kohlstedt. 2003
267 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/5da00fb4ce64f8a689926324de62ba0ce8cd842f
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In Geophysics
Citations in the corpus
- Organized melt, seismic anisotropy, and plate boundary lubrication (2010, background): “In laboratory experiments, differential stress causes melt to align and organize into networks of melt‐rich shear zones [e.g.,Holtzman et al., 2003b], leading to significant strain weakening [e.g., Holtzman and Kohlstedt, 2007; King et al., 2010].”
- Viscous constitutive relations of solid-liquid composites in terms of grain boundary contiguity: 1. Grain boundary diffusion control model (2009, background): “These observations include both grain-scale melt alignment in compression [Daines and Kohlstedt, 1997], pure shear [Takei, 2005] and simple shear [Zimmerman et al., 1999], and also melt redistribution over distances greater than the grain scale into networks of melt-rich shear zones [ Holtzman et al”
- Rheology of the Earth's mantle: A historical review (2010, background): “Knowing the problems of compaction, they argued that melt-rich layers occur as horizontal thin channels and these layers are isolated citing the results of study by Holtzman et al. (2003a,b). However, the plausibility of such a structure is questionable because, according to the study by Holtzman et”
- Numerical modelling of magma dynamics coupled to tectonic deformation of lithosphere and crust (2013, background): “Also, the melt bands observed in analogue simple shear experiments form at angles of 55◦–70◦ to the least compressive stress direction (Holtzman 2003).”
- Shearing Melt Out of the Earth: An Experimentalist's Perspective on the Influence of Deformation on Melt Extraction (2009, background): “This situation arises because of the strong dependence of compaction length on melt fraction, as illustrated in figure 7 of Holtzman et al. (2003a).”
- Fate of Pyroxenite-derived Melts in the Peridotitic Mantle: Thermodynamic and Experimental Constraints (2012, background): “Sleep,1988; Takahashi, 1992); (3) mechanical stress-driven localization of melt (Holtzman et al., 2003); (4) presence of a barrier to upward melt migration at the base of the oceanic lithosphere (e.”