Abstract | Keywords | Export | Availability | Bookmark

Choose an application

• Reference Manager
• EndNote
• RefWorks (Direct export to RefWorks)

Mathematical Modeling of Earth's Dynamical Systems gives earth scientists the essential skills for translating chemical and physical systems into mathematical and computational models that provide enhanced insight into Earth's processes. Using a step-by-step method, the book identifies the important geological variables of physical-chemical geoscience problems and describes the mechanisms that control these variables. This book is directed toward upper-level undergraduate students, graduate students, researchers, and professionals who want to learn how to abstract complex systems into sets of dynamic equations. It shows students how to reorganize domains of interest and key factors, and how to explain assumptions in formal terms. The book reveals what data best tests ideas of how nature works, and cautions against inadequate transport laws, unconstrainec coeffecients, and unfalsifiable models. Studentr using this text should be familiar with the principles of physics, chemistry, and geology, and have taken a year of differential and integral calculus. -- BACK COVER

Gaia hypothesis --- 551.24 --- 551.24 Geotectonics. Crust movements. Tectonic structures and their elements.Faults.Folds. Uplift. Subsidence. Compression. Tectogenesis. Orogenesis. --- Geotectonics. Crust movements. Tectonic structures and their elements.Faults.Folds. Uplift. Subsidence. Compression. Tectogenesis. Orogenesis. --- Gaia concept --- Gaia principle --- Gaia theory --- Gaian hypothesis --- Living earth theory --- Ecology --- Geobiology --- Biosphere --- Mathematical models. --- Philosophy --- Hypothèse Gaïa --- Mathematical models --- Modèles mathématiques --- Gaia hypothesis - Mathematical models. --- Gaia hypothesis --Mathematical models. --- Geobiology. --- Biology --- Earth sciences --- Geotectonics. Crust movements. Tectonic structures and their elements.Faults.Folds. Uplift. Subsidence. Compression. Tectogenesis. Orogenesis