Oxford University Press, 08.09.1994 - 411 Seiten
This monograph offers an interdisciplinary approach to the analysis of geological systems which become spatially organized through the mediation of chemical processes. The treatment is based on a mathematical approach. The intended readership includes researchers and advanced undergraduate and graduate students in all branches of geology as well as scientists and mathematicians concerned with nonlinear dynamics, numerical analysis, self-organization, nonlinear waves and dynamics, and phase transition phenomena. The work could also serve as a basis for a special topics course in mathematics, chemistry or physics.
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Feedback Instability and Bifurcation
Oscillatory Zoning In Crystals
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advection amplitude analysis assumed bands behavior bifurcation theory boundary conditions calcite cementation Chadam Chapter chemical compaction complex concentration crystal deformation denoted dependence descriptive variables diagenesis diagenetic dissolution front distribution domain dynamics equations equilibrium constant evolution example feedback flow fluid pressure formula units fracture free energy gradient grain growth growing hence instability interface kerogen kinetics layering Liesegang linear macroscopic macrovolume element matrix mechanism mechanochemical medium metamorphic differentiation metamorphic rocks mineral molar density monomer muscovite nonequilibrium nonlinear nucleation obtained Ortoleva oscillation oscillatory zoning parameter particle patterns permeability perturbations phenomena planar pore fluid porosity porous porous medium preceding precipitate pressure solution problem processes profiles quartz radius rate coefficient rate law reaction front reaction-transport region rock sandstone scale seal Section sedimentary self-organization solid spatial stability stoichiometric coefficient stress structure stylolites suggested in Fig surface temperature texture theory tion variations vector velocity wavelength yields