Lingua: Inglese
Editore: Geological Society of London, 2012
ISBN 10: 1862393389 ISBN 13: 9781862393387
Da: Revaluation Books, Exeter, Regno Unito
EUR 225,63
Quantità: 1 disponibili
Aggiungi al carrelloHardcover. Condizione: Brand New. 204 pages. 10.25x6.75x1.00 inches. In Stock.
Lingua: Inglese
Editore: Geological Society Of London, 2011
ISBN 10: 1862393389 ISBN 13: 9781862393387
Da: Mispah books, Redhill, SURRE, Regno Unito
EUR 237,30
Quantità: 1 disponibili
Aggiungi al carrelloHardcover. Condizione: Like New. LIKE NEW. SHIPS FROM MULTIPLE LOCATIONS. book.
Da: ECOSPHERE, Champs sur marne, Francia
EUR 199,00
Quantità: 1 disponibili
Aggiungi al carrelloCouverture rigide. Condizione: Neuf.
Lingua: Inglese
Editore: Geological Society Of London, 2011
ISBN 10: 1862393389 ISBN 13: 9781862393387
Da: Joseph Burridge Books, Dagenham, Regno Unito
EUR 262,34
Quantità: 1 disponibili
Aggiungi al carrelloThis 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.