Magma flow through elastic-walled dikes
A convection–diffusion model for the averaged flow of a viscous, incompressible magma through an elastic medium is considered. The magma flows through a dike from a magma reservoir to the Earth’s surface; only changes in dike width and velocity over large vertical length scales relative to the chara...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Springer
2005
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Subjects: | |
Online Access: | http://purl.utwente.nl/publications/61962 |