Abstract
Brucite was investigated by Raman spectroscopy to pressures of 36.6 GPa under nonhydrostatic conditions and to 19.7 GPa under quasi-hydrostatic conditions. Several new Raman lines are first observed at 4 GPa, demonstrating the existence of a high-pressure structural change. Raman data are compared with recent infrared spectroscopy, X-ray diffraction, and neutron diffraction studies of brucite. The structural change is likely to involve displacement or disordering of the H atoms, consistent with neutron diffraction results. -from Authors
Original language | English (US) |
---|---|
Pages (from-to) | 222-230 |
Number of pages | 9 |
Journal | American Mineralogist |
Volume | 80 |
Issue number | 3-4 |
DOIs | |
State | Published - 1995 |
Externally published | Yes |
All Science Journal Classification (ASJC) codes
- Geophysics
- Geochemistry and Petrology