Many faults appear to form persistent zones of weakness that fundamentally influence the distribution, architecture and movement patterns of crustal-scale deformation and associated process in both continental and oceanic regions. This book brings together papers by an international group of Earth Scientists to discuss a broad range of topics centred upon the controls of fault weakening and the role of such faults during lithosphere deformation. Readership:Academic structural-tectonic geologists, microstructural geologists, rheologists, geophysicists and people studying geodynamics. Also, petroleum geologists, hardrock geologists, mining geologists, hydrogeologists and metamorphic geologists. Suitable for postgraduate students.

Also available:

Exhumation Processes: Normal Faulting, Ductile Flow and Erosion (Geological Society Special Publication) - ISBN 1862390320
The Internal Structure of Fault Zones: Implications for Mechanical & Fluid-Flow Properties - Special Publication no 299 - ISBN 1862392536

The Geological Society of London

Founded in 1807, the Geological Society of London is the oldest geological society in the world, and one of the largest publishers in the Earth sciences.

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