Melting and channelized magmatic flow in chemically heterogeneous, upwelling mantle
- 2 May 2012
- journal article
- Published by American Geophysical Union (AGU) in Geochemistry, Geophysics, Geosystems
- Vol. 13 (5)
- https://doi.org/10.1029/2011gc003989
Abstract
No abstract availableKeywords
This publication has 81 references indexed in Scilit:
- The energetics of melting fertile heterogeneities within the depleted mantleGeochemistry, Geophysics, Geosystems, 2011
- Porosity‐driven convection and asymmetry beneath mid‐ocean ridgesGeochemistry, Geophysics, Geosystems, 2010
- Numerical simulation of geodynamic processes with the Portable Extensible Toolkit for Scientific ComputationPhysics of the Earth and Planetary Interiors, 2007
- FOZO, HIMU, and the rest of the mantle zooGeochemistry, Geophysics, Geosystems, 2005
- Flow and melting of a heterogeneous mantle: 1. Method and importance to the geochemistry of ocean island and mid-ocean ridge basaltsEarth and Planetary Science Letters, 2005
- Chemical and seismological constraints on mantle heterogeneityPhilosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 2002
- A two‐phase model for compaction and damage: 1. General TheoryJournal of Geophysical Research, 2001
- Melting enthalpies of mantle peridotite: calorimetric determinations in the system CaO-MgO-Al2O3-SiO2 and application to magma generationEarth and Planetary Science Letters, 1997
- Mathematical Modeling of Melting and Freezing ProcessesJournal of Solar Energy Engineering, 1993
- A mathematical model of magma transport in the asthenosphereGeophysical & Astrophysical Fluid Dynamics, 1985