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Post-Perovskite : the Last Mantle Phase Transition.

Published by the American Geophysical Union as part of the Geophysical Monograph Series. 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 experim...

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Bibliographic Details
Call Number:Libro Electrónico
Main Author: Hirose, Katsuhiko
Other Authors: Brodholt, J., Lay, T., Yuen, D. A.
Format: Electronic eBook
Language:Inglés
Published: Washington : Wiley, 2013.
Series:Geophysical monograph ; 174.
Subjects:
Online Access:Texto completo
Table of Contents:
  • Title Page; Contents; Preface; An Introduction to Post-Perovskite: The Last Mantle Phase Transition; Section I: Mineral Physics (Experimental); Review of Experimental Studies on Mantle Phase Transitions; Discovery of Post-Perovskite Phase Transition and the Nature of D. Layer; Effect of Iron on the Properties of Post-Perovskite Silicate; Electronic Transitions and Spin States in the Lower Mantle; Lattice-Preferred Orientation of Lower Mantle Materials and Seismic Anisotropy in the D. Layer; Section II: Mineral Physics (Theoretical)
  • Thermodynamic Properties and Stability Field of MgSiO3 Post-PerovskiteThe High-Temperature Elasticity of MgSiO3 Post-Perovskite; Effect of Chemistry on the Physical Properties of Perovskite and Post-Perovskite; Section III: Seismology; Reconciling the Post-Perovskite Phase With Seismological Observations of Lowermost Mantle Structure; Predicting a Global Perovskite and Post-Perovskite Phase Boundary; Seismic Anisotropy of Post-Perovskite and the Lowermost Mantle; Constraints on the Presence or Absence of Post-Perovskite in the Lowermost Mantle From Long-Period Seismology; Section IV: Dynamics
  • Mantle Dynamics and the D"" Layer: Impacts of the Post Perovskite PhaseInfluence of the Post-Perovskite Transition on Thermal and Thermo-Chemical Mantle Convection; The Dynamical Influences From Physical Properties in the Lower Mantle and Post-Perovskite Phase Transition; Deformation-Induced Mechanical Instabilities at the Core-Mantle Boundary