A two-dimensional model for magma ascent in volcanic conduits is presented. The model accounts for the magma rheology, heat flux to the surrounding country rock, planar and axisymmetric geometries, and flow in the mushy region by means of a continuum mixture formulation that does not require keeping
Ascent of Bubbles in Magma Conduits Using Boundary Elements and Particles
β Scribed by Gabriele Morra; Leonardo Quevedo; Dave A. Yuen; Philippe Chatelain
- Book ID
- 108255602
- Publisher
- Elsevier
- Year
- 2011
- Tongue
- English
- Weight
- 334 KB
- Volume
- 4
- Category
- Article
- ISSN
- 1877-0509
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