Eiichi Fukuyama – författare

The dynamics of the earthquake rupture process are closely related to fault zone properties which the authors have intensively investigated by various observations in the field as well as by laboratory experiments. These include geological investigation of the active and fossil faults, physical and chemical features obtained by the laboratory experiments, as well as the seismological estimation from seismic waveforms. Earthquake dynamic rupture can now be modeled using numerical simulations on the basis of field and laboratory observations, which should be very useful for understanding earthquake rupture dynamics.Features:First overview of new and improved techniques in the study of earthquake faultingBroad coverageFull colorBenefits:A must-have for all geophysicists who work on earthquake dynamicsSingle resource for all aspects of earthquake dynamics (from lab measurements to seismological observations to numerical modelling)Bridges the disciplines of seismology, structural geology and rock mechanicsHelps readers to understand and interpret graphs and mapsAlso has potential use as a supplementary resource for upper division and graduate geophysics courses.

This book presents a series of numerical simulation studies of the earthquake generation process and the evaluation of the hazards caused by large earthquakes and tsunamis, drawn from three distinct topical areas. First, recent research results on earthquake source physics are introduced, which can be used as input for hazard evaluation studies. Then, propagation of seismic waves and tsunamis is discussed, connecting what happens at the source with the resulting damage. Finally, earthquake statistics for forecasting are discussed, a practical application of our knowledge for the mitigation of earthquake and tsunami disasters.This book is suitable for graduate students who are interested in the earthquake generation process and its application in the future. It also will serve researchers who want or need to know how to evaluate the damage due to earthquakes and tsunamis.