The effect of effective rock viscosity on 2-D magmatic porosity waves
<p>In source regions of magmatic systems the temperature is above solidus, and melt ascent is assumed to occur predominantly by two-phase flow, which includes a fluid phase (melt) and a porous deformable matrix. Since McKenzie (1984) introduced equations for two-phase flow, numerous solutions...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2019-12-01
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| Series: | Solid Earth |
| Online Access: | https://www.solid-earth.net/10/2103/2019/se-10-2103-2019.pdf |