Isostasy and Flexure of the Lithosphere
Autor A. B. Wattsen Limba Engleză Paperback – 29 sep 2023
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Specificații
ISBN-13: 9781009278928
ISBN-10: 1009278924
Pagini: 520
Dimensiuni: 244 x 170 x 37 mm
Greutate: 1.18 kg
Ediția:2Revizuită
Editura: Cambridge University Press
Colecția Cambridge University Press
Locul publicării:Cambridge, United Kingdom
ISBN-10: 1009278924
Pagini: 520
Dimensiuni: 244 x 170 x 37 mm
Greutate: 1.18 kg
Ediția:2Revizuită
Editura: Cambridge University Press
Colecția Cambridge University Press
Locul publicării:Cambridge, United Kingdom
Cuprins
1. The Development of the Concept of Isostasy; 2. Isostasy and Flexure of the Lithosphere; 3. Theory of Elastic Plates; 4. Geological Examples of the Flexure Model of Isostasy; 5. Isostatic Response Functions; 6. Isostasy and the Physical Nature of the Lithosphere; 7. Isostasy and the Origin of Geological Features in the Continents and Oceans; 8. Isostasy and the Terrestrial Planets; References; Index.
Recenzii
'The second edition of this classic book offers an in-depth analysis of the numerous land, ocean, and planetary processes that are produced and modified by lithospheric flexure. Topics range from the theory of bending and deformation of thin elastic plates, to the relationships between gravity and topography, to the interaction of flexural and erosional processes and their geological interpretation. Throughout the book there are sections on the historical developments of all these topics. This new edition includes updates on yield strength envelope models for the lithosphere and the interpretation of new gravity and topography measured by satellite missions orbiting the Earth and other planets. Whether you are a geologist, geophysicist, or simply an enthusiast seeking a deeper understanding of the Earth's geological processes, Isostasy and Flexure of the Lithosphere is an invaluable resource.' David Sandwell, University of California, San Diego
Descriere
A unique overview of isostasy featuring recent advances in spectral data analysis and understanding of variations in lithospheric strength.