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...

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Bibliographic Details
Main Authors: Bokhove, O., Woods, A.W., Boer, A. de
Format: Article in Journal/Newspaper
Language:unknown
Published: Springer 2005
Subjects:
Online Access:http://purl.utwente.nl/publications/61962