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The Nature and Tectonic Significance of Fault Zone Weakening
Many faults appears to form persistent zones of weakness that fundamentally influence the distribution, arichitecture and movement patterns of crustal-scale deformation and associated processes in both continental and oceanic regions. They act as conduits for the focused migration of economically important fluids and also constitute one of the most important global geological hazards. 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.
The Geometry and Growth of Normal Faults
Normal faults are the primary structures that accommodate extension of the brittle crust. This volume provides an up-to-date overview of current research into the geometry and growth of normal faults. The 23 research papers present the findings of outcrop and subsurface studies of the geometrical evolution of faults from a number of basins worldwide, complemented by analogue and numerical modelling studies of fundamental aspects of fault kinematics. The topics addressed include how fault length changes with displacement, how faults interact with one another, the controls of previous structure on fault evolution and the nature and origin of fault-related folding. This volume will be of interest to those wishing to develop a better understanding of the structural geological aspects of faulting, from postgraduate students to those working in industry.
Continental Transpressional and Transtensional Tectonics
Many present-day and ancient continental deformation systems appear to have formed due to significantly oblique relative plate motions. Transpression and transtension zones are formed where the oblique motions involve components of compression and extensions, respectively. This book covers the recent advances in our understanding or transpressional and transtensional deformation zones both in theory and in real geological settings from around the world. The volume opens with an up-to-date overview of the topic that sets the scene for the more detailed papers which follow. The papers are grouped into four sections. The first, Modelling Transpression and Transtension, includes a series of pape...
Solid Geology of the Tongue District
This memoir describes the solid geology of the district which lies to the east of Cape Wrath, near the north-west extremity of mainland Scotland. Geologically, the district is important for its position at the western margin of the Caledonian mountain chain, and for the fact that the coast provides a good cross-section across that margin.
Continental Transpressional Tectonics and Transtensional Tectonics
Many present-day and ancient continental deformation systems appear to have formed due to significantly oblique relative plate motions. Transpression and transtension zones are formed where the oblique motions involve components of compression and extensions, respectively. This book covers the recent advances in our understanding or transpressional and transtensional deformation zones both in theory and in real geological settings from around the world.
