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Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 174.

Discovery of the perovskite to post-perovskite phase transition in MgSiO3, expected to occur for deep mantle conditions, was first announced in April 2004. This immediately stimulated numerous studies in experimental and theoretical mineral physics, seismology, and geodynamics evaluating the implications of a major lower mantle phase change. A resulting revolution in our understanding of the D? region in the lowermost mantle is well underway. This monograph presents the multidisciplinary advances to date ensuing from interpreting deep mantle seismological structures and dynamical processes in the context of the experimentally and theoretically determined properties of the post-perovskite phase change; the last silicate phase change likely to occur with increasing pressure in lowermost mantle rocks.
Pages
287 pages
Collection
Geophysical Monograph Series
Parution
2013-04-30
Marque
American Geophysical Union
EAN papier
9780875904399
EAN PDF
9781118672495

Informations sur l'ebook
Nombre pages copiables
0
Nombre pages imprimables
287
Taille du fichier
42527 Ko
Prix
120,22 €
EAN EPUB
9781118671931

Informations sur l'ebook
Nombre pages copiables
0
Nombre pages imprimables
287
Taille du fichier
7916 Ko
Prix
120,22 €