This book investigates the complex rheological properties and deformation mechanisms of the lithosphere specifically at continental margins. Brian Taylor, drawing on extensive geophysical and geological data, presents a comprehensive analysis of how the Earth's crust and upper mantle behave under the stresses associated with plate tectonics at these critical transition zones. The work synthesizes current understanding of rock mechanics, seismic data, and modeling to explain the observed geological structures and processes.

This text is recognized as a significant contribution to the field of geodynamics, particularly for its focus on continental margins. Experts in the field likely regard it as a valuable resource for understanding the physical processes governing these complex geological environments. The book's detailed approach and integration of diverse data sets suggest it is aimed at advanced students and researchers in geophysics and geology.