Stress‐induced anisotropy of partially molten media inferred from experimental deformation of a simple binary system under acoustic monitoring
- 10 January 2001
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 106 (B1) , 567-588
- https://doi.org/10.1029/2000jb900361
Abstract
No abstract availableKeywords
This publication has 34 references indexed in Scilit:
- Granitic magma transport by fracture propagationPublished by Elsevier ,2003
- Influence of deformation on melt topology in peridotitesJournal of Geophysical Research, 1997
- Experimental constraints on the dynamics of the partially molten upper mantle: 2. Deformation in the dislocation creep regimeJournal of Geophysical Research, 1995
- Experimental constraints on the dynamics of the partially molten upper mantle: Deformation in the diffusion creep regimeJournal of Geophysical Research, 1995
- Temperature and pressure dependence of quartz-aqueous fluid dihedral angles: the control of adsorbed H2O on the permeability of quartzitesEarth and Planetary Science Letters, 1993
- A thermodynamic analysis of the conditions of equilibrium at nonhydrostatically stressed and curved solid‐fluid interfacesJournal of Geophysical Research, 1991
- Textural Development and Melt Topology in Spinel Lherzolite Experimentally Deformed at Hypersolidus ConditionsJournal of Petrology, 1991
- Rheology and structure of olivine‐basalt partial meltsJournal of Geophysical Research, 1986
- Mathematical Modeling of Two-Phase FlowAnnual Review of Fluid Mechanics, 1983
- Mechanical and thermodynamic constraints on fluid distribution in partial meltsJournal of Geophysical Research, 1979