Flow Processes in Faults And Shear Zones (Geological Society Special Publication) (No. 224)

G. I. Alsop

ISBN 10: 186239153X / ISBN 13: 9781862391536

Published by Geological Society of London, 2004

About this Item

Faults and their deeper level equivalents, shear zones, are localized regions of intense deformation within the Earth. They are recognized at all scales from micro to plate boundary, and are important examples of the nature of heterogeneous deformation in natural rocks. Faults and shear zones are significant as they profoundly influence the location, architecture and evolution of a broad range of geological phenomena. The topography and bathymetry of the Earth?s surface is marked by mountain belts and sedimentary basins which are controlled by faults and shear zones. In addition faults and shear zones control fluid migration and transport including hydrothermal and hydrocarbon systems. Once faults and shear zones are established, they are often long-lived features prone to multiple reactivation over very large time-scales. This collection of papers addresses lithospheric deformation and the rheology of shear zones, together with processes of partitioning and the unravelling of fault and shear zone histories.

Seller Inventory # PGGEOXX140

Bibliographic Details

• Title: Flow Processes in Faults And Shear Zones (Geological Society Special Publication) (No. 224)
• Publisher: Geological Society of London
• Publication Date: 2004
• Language: English
• ISBN 10: 186239153X
• ISBN 13: 9781862391536
• Binding: Hardcover
• Condition: New
• Dimensions: 17.15W x 24.77H x 2.54D centimeters 17.15 centimeters width by 24.77 centimeters height by 2.54 centimeters depth
• Weight: 953 grams

About this title

Synopsis

Faults and their deeper level equivalents, shear zones, are localized regions of intense deformation within the Earth. They are recognized at all scales from micro to plate boundary, and are important examples of the nature of heterogeneous deformation in natural rocks. Faults and shear zones are significant as they profoundly influence the location, architecture and evolution of a broad range of geological phenomena. The topography and bathymetry of the Earth's surface is marked by mountain belts and sedimentary basins which are controlled by faults and shear zones. In addition faults and shear zones control fluid migration and transport including hydrothermal and hydrocarbon systems. Once faults and shear zones are established, they are often long-lived features prone to multiple reactivation over very large time-scales. This collection of papers addresses lithospheric deformation and the rheology of shear zones, together with processes of partitioning and the unravelling of fault and shear zone histories.

Also available:

The Internal Structure of Fault Zones: Implications for Mechanical & Fluid-Flow Properties - Special Publication no 299 - ISBN 1862392536
Tectonics of Strike-Slip Restraining and Releasing Bends - Special Publication no 290 - ISBN 1862392382

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