Idioma: Inglés
Publicado por Geological Society of London, 2012
ISBN 10: 1862393389 ISBN 13: 9781862393387
Librería: Revaluation Books, Exeter, Reino Unido
EUR 225,56
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Añadir al carritoHardcover. Condición: Brand New. 204 pages. 10.25x6.75x1.00 inches. In Stock.
Idioma: Inglés
Publicado por Geological Society Of London, 2011
ISBN 10: 1862393389 ISBN 13: 9781862393387
Librería: Mispah books, Redhill, SURRE, Reino Unido
EUR 236,56
Cantidad disponible: 1 disponibles
Añadir al carritoHardcover. Condición: Like New. LIKE NEW. SHIPS FROM MULTIPLE LOCATIONS. book.
Librería: ECOSPHERE, Champs sur marne, Francia
EUR 199,00
Cantidad disponible: 1 disponibles
Añadir al carritoCouverture rigide. Condición: Neuf.
Idioma: Inglés
Publicado por Geological Society Of London, 2011
ISBN 10: 1862393389 ISBN 13: 9781862393387
Librería: Joseph Burridge Books, Dagenham, Reino Unido
EUR 261,53
Cantidad disponible: 1 disponibles
Añadir al carritoThis collection of papers presents recent advances in the study of deformation mechanisms and rheology and their applications to tectonics. Many of the contributions exploit new petrofabric techniques, particularly electron backscatter diffraction, to help understand the evolution of rock microstructure and mechanical properties. Papers in the first section (lattice preferred orientations and anisotropy ) show a growing emphasis on the determination of elastic properties from petrofabrics, from which acoustic properties can be computed for comparison with in-situ seismic measurements. Such research will underpin geodynamic interpretation of large-scale active tectonics. Contributions in the second section (microstructures, mechanisms and rheology) study the relations between microstructural evolution during deformation and mechanical properties. Many of the papers explore how different mechanisms compete and interact to control the evolution of grain size and petrofabrics. Contributors make use of combinations of laboratory experiments, field studies and computational methods, and several relate microstructural and mechanical evolution to large-scale tectonic processes observed in nature.