Magmons: Solitary Waves Arising in the Buoyant Ascent of Magma by Porous Flow through a Viscously Deformable Matrix

Magmons: Solitary Waves Arising in the Buoyant Ascent of Magma by Porous Flow through a Viscously Deformable Matrix

<p>The dynamics of partially molten regions of the Earth's mantle are studied using a combination of theoretical, experimental, and numerical techniques. The physical model is based on experimental observations of partially molten ultramafic rocks and incorporates two elements: buoyancy-d...

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Bibliographic Details
Main Author: Scott, David Russell
Format: Others
Language:en
Published: 1987
Online Access:https://thesis.library.caltech.edu/11448/2/Scott_DR_1987.pdf
Scott, David Russell (1987) Magmons: Solitary Waves Arising in the Buoyant Ascent of Magma by Porous Flow through a Viscously Deformable Matrix. Dissertation (Ph.D.), California Institute of Technology. doi:10.7907/mvdj-ty73. https://resolver.caltech.edu/CaltechTHESIS:04052019-172938000 <https://resolver.caltech.edu/CaltechTHESIS:04052019-172938000>

Internet

https://thesis.library.caltech.edu/11448/2/Scott_DR_1987.pdf
Scott, David Russell (1987) Magmons: Solitary Waves Arising in the Buoyant Ascent of Magma by Porous Flow through a Viscously Deformable Matrix. Dissertation (Ph.D.), California Institute of Technology. doi:10.7907/mvdj-ty73. https://resolver.caltech.edu/CaltechTHESIS:04052019-172938000 <https://resolver.caltech.edu/CaltechTHESIS:04052019-172938000>

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