tectonic belts originate through a single mechanism and that this mechanism can be described in terms of the laws of physics, especially Newton's three laws of motion, and their derivatives - Pascal's law, Stokes's law, the Peach-Köhler force (a derivative of the law of gravity), Poiseuille's law, the Navier-Stokes equations and the Navier-Coulomb maximum stress theory. This book will be of interest to scientists and researchers in many disciplines, not just geology and geophysics, but also fluid mechanics and related fields. The targeted audience includes advanced geology and geophysics majors, graduate students at all levels and all persons involved in structural geology, tectonics, igneous geochemistry and mineral exploration.

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