Titlebook: Very Slow Flows of Solids; Basics of Modeling i Louis A. Lliboutry Book 1987 Martinus Nijhoff Publishers, Dordrecht 1987 Deformation.contin

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of igneous, volcanic, sedimentary, and metamorphic rocks of Archaean and Precambrian age. In this terrain the aquifers are characteristically thin, discontinuous, of irregular occurrence, and hence of low to moderate yield potentials. The latter depends mainly on the distribution of porosity, impart

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https://doi.org/10.1007/978-94-009-3563-1Deformation; continuum mechanics; dynamics; elasticity; finite element method; geodynamics; matrix; mechani

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Numerical simulation of very slow flows: an overview,In the development of a discipline three stages may be recognized [1].

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反對

,Thermal convection in an isoviscous layer and in the Earth’s mantle,The density of the solid medium has been hitherto considered as a constant. In fact, in real media it depends somewhat on pressure . because the medium always has an elastic behavior (superimposed on the viscosity that we are considering), and on temperature ..

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Computation of very slow flows by the finite-difference method,The computation of steady coupled velocity and temperature fields can be done in two ways:

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