Titlebook: Earth Sciences and Mathematics, Volume II; Antonio G. Camacho,Jesús I. Díaz,José Fernändez Book 2009 Birkhäuser Basel 2009 Deformation.Ear

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On the Mathematical Analysis of an Elastic-gravitational Layered Earth Model for Magmatic Intrusion strain in layered linear elastic-gravitational media. The approximation of the solution for the half space was obtained by using the propagator matrix technique. The Earth model considered is elastic-gravitational, composed of several homogeneous layers overlying a bottom half space. Two dislocatio

Terminal

Modelling Gravitational Instabilities: Slab Break-off and Rayleigh-Taylor Diapirism,d in the code are described: A level set technique to track the position of the materials and an enrichment of the solution to allow the strain rate to be discontinuous across the interface. These techniques have low computational cost and can be used in standard desktop PCs. Examples of phase track

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On the Coupling Between Channel Level and Surface Ground-Water Flows,us flows of surface, soil and ground waters. Such models are widely used for forecasting (numerical simulation) of a hydrological cycle for concrete territories. The mathematical models that proved a more realistic approach are obtained by combining several mathematical models for local processes. T

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A Mathematical Study of the Ice Flow Behavior in a Neighborhood of the Grounding Line,n the motion of glaciers. It is widely assumed that the stability of the marine ice sheets, as in the West Antarctic Ice Sheet (WAIS), where ice shelves are formed, is mainly controlled by the dynamics of the grounding line. The grounding line is the line where transition between ice attached to the

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Potential Symmetry Properties of a Family of Equations Occuring in Ice Sheet Dynamics,mation in glaciology. In addition we present a classical potential symmetry analysis of this second-order nonlinear degenerate parabolic equation related to non- Newtonian ice sheet dynamics in the isothermal case. After obtaining a general result connecting the thickness function of the ice sheet a