Language: English
Published by Geological Society of London, 1999
ISBN 10: 1862390320 ISBN 13: 9781862390324
Seller: HPB-Red, Dallas, TX, U.S.A.
Hardcover. Condition: Good. Connecting readers with great books since 1972! Used textbooks may not include companion materials such as access codes, etc. May have some wear or writing/highlighting. We ship orders daily and Customer Service is our top priority!
Language: English
Published by Geological Society of London, 1999
ISBN 10: 1862390320 ISBN 13: 9781862390324
Seller: Phatpocket Limited, Waltham Abbey, HERTS, United Kingdom
Condition: Good. Your purchase helps support Sri Lankan Children's Charity 'The Rainbow Centre'. Ex-library, so some stamps and wear, but in good overall condition. Our donations to The Rainbow Centre have helped provide an education and a safe haven to hundreds of children who live in appalling conditions.
Language: English
Published by Geological Society Pub House, 1999
ISBN 10: 1862390320 ISBN 13: 9781862390324
Seller: Revaluation Books, Exeter, United Kingdom
Hardcover. Condition: Brand New. illustrated edition. 378 pages. 10.25x7.25x1.00 inches. In Stock.
Language: English
Published by Geological Society of London, 1999
ISBN 10: 1862390320 ISBN 13: 9781862390324
Seller: Joseph Burridge Books, Dagenham, United Kingdom
Hardcover. Condition: New. The book will be a broad interest to any student of mountain belts and orogenesis, including those in tectonics, structural geology, geodynamics, metamorphic petrology, sedimentology and geomorphology. Field geology is, by definition, the geology of exhumed rocks. This book provides a broad range of examples of deep exhumation and emphasizes the competition between the various exhumation processes: normal faulting, ductile thinning and erosion. The papers include examples from all parts of the world and from a variety of tectonic settings, including oceanic subduction zones, continental collision zones and continental rifts. The volume explores the relationship between climate, erosion and tectonics. It provides innovative applications of thermochronology to understanding the rates and geometry of normal faulting, and the interaction between erosion and tectonics.