Modeling liquid transport in the Earth's mantle as two-phase flow: effect of an enforced positive porosity on liquid flow and mass conservation
Fluid and melt transport in the solid mantle can be modeled as a two-phase flow in which the
liquid flow is resisted by the compaction of the viscously deforming solid mantle. Given the …
liquid flow is resisted by the compaction of the viscously deforming solid mantle. Given the …