Magma ascent mechanisms in the transition regime from solitary porosity waves to diapirism
<p>In partially molten regions inside the Earth, melt buoyancy may trigger upwelling of both solid and fluid phases, i.e., diapirism. If the melt is allowed to move separately with respect to the matrix, melt perturbations may evolve into solitary porosity waves. While diapirs may form on a wi...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2021-07-01
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| Series: | Solid Earth |
| Online Access: | https://se.copernicus.org/articles/12/1549/2021/se-12-1549-2021.pdf |