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University of Cambridge > Talks.cam > Isaac Newton Institute Seminar Series > Geodynamics and Two-Phase Flow: A Computational Perspective
Geodynamics and Two-Phase Flow: A Computational PerspectiveAdd to your list(s) Download to your calendar using vCal
If you have a question about this talk, please contact INI IT. This talk has been canceled/deleted The system of partial differential equations used in geodynamic contexts to study melt migration define the evolution of a two-phase system comprised of a highly viscous, porous crystalline mantle rock (“solid” phase) through which low viscosity magma (“fluid” phase) can flow. Typical geodynamic two-phase flow scenarios are characterized by rheological non-linearities, localization and flows possessing a range of characteristic length scales. This talk is part of the Isaac Newton Institute Seminar Series series. This talk is included in these lists:This talk is not included in any other list Note that ex-directory lists are not shown. |
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