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Attempts to answer such concerns as why some interplate subduction earthquakes are modest in rupture length, while others rupture along 1000 km or more. This book addresses why certain subduction zones are locked, accumulating elastic strain at essentially the full plate convergence rate, while others appear to be coupled or even freely slipping.
This book explores the current cutting-edge interdisciplinary research in lithospheric rheology and provides a broad summary of the rheology and deformation of the continental lithosphere in both extensional and compressional settings. Individual chapters explore contemporary research resulting from laboratory, observational, and theoretical experiments.
This book explores the current cutting-edge interdisciplinary research in lithospheric rheology and provides a broad summary of the rheology and deformation of the continental lithosphere in both extensional and compressional settings. Individual chapters explore contemporary research resulting from laboratory, observational, and theoretical experiments.
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