Choose an application

• Reference Manager
• EndNote
• RefWorks (Direct export to RefWorks)

High-pressure mineral physics is a field that is strongly driven by the development of new technology. Fifty years ago, when experimentally achievable pressures were limited to just 25 GPa, little was know about the mineralogy of the Earth's lower mantle. Silicate perovskite, the likely dominant mineral of the deep Earth, was identified only when the high-pressure techniques broke the pressure barrier of 25 GPa in 1970's. However, as the maximum achievable pressure reached beyond one Megabar (100 GPa) and even to the pressure of Earth's core on minute samples, new discoveries increasingly were

Mineralogy. --- Mineralogical chemistry. --- Geophysics. --- Materials at high pressures.

Choose an application

• Reference Manager
• EndNote
• RefWorks (Direct export to RefWorks)

Volume 37 of Reviews in Mineralogy, divided into three sections, begins with an overview (Chapter 1) of the remarkable advances in the ability to subject minerals-not only as pristine single-crystal samples but also complex, natural mineral assemblages-to extreme pressure-temperature conditions in the laboratory. These advances parallel the development of an arsenal of analytical methods for measuring mineral behavior under those conditions. This sets the stage for section two (Chapters 2-8) which focuses on high-pressure minerals in their geological setting as a function of depth. This top-down approach begins with what we know from direct sampling of high-pressure minerals and rocks brought to the surface to detailed geophysical observations of the vast interior. The third section (Chapters 9-19) presents the material fundamentals, starting from properties of a chemical nature, such as crystal chemistry, thermochemistry, element partitioning, and melting, and moving toward the domain of mineral physics such as melt properties, equations of state, elasticity, rheology, vibrational dynamics, bonding, electronic structure, and magnetism. The Review thus moves from the complexity of rocks to their mineral components and finally to fundamental properties arising directly from the play of electrons and nuclei.This volume was prepared for a short course by the same title, organized by Russell J. Hemley and Ho-kwang Mao and sponsored by the Mineralogical Society of America, December 4-6, 1998 on the campus of the University of California at Davis.

Mineralogy. --- Materials at high pressures. --- Earth (Planet) --- Mantle. --- Core.

Choose an application

• Reference Manager
• EndNote
• RefWorks (Direct export to RefWorks)

High pressure (Science) --- Experiments --- Technique --- Materials at high pressures --- High pressure (Science) - Experiments - Technique. --- Materials at high pressures - Experiments - Technique.

Choose an application

• Reference Manager
• EndNote
• RefWorks (Direct export to RefWorks)

High pressure (Science). --- Materials at high pressures. --- Phase transformations (Statistical physics). --- Surface chemistry. --- Surfaces (Physics).

Choose an application

• Reference Manager
• EndNote
• RefWorks (Direct export to RefWorks)

Hard materials --- Materials at high pressures --- Graphite --- Mechanical properties --- Research. --- Research. --- Properties.