Phase transformations in serpentine and transportation of water into the lower mantle
- 15 January 1998
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 25 (2) , 203-206
- https://doi.org/10.1029/97gl03572
Abstract
No abstract availableThis publication has 23 references indexed in Scilit:
- Structure and crystal chemistry of Phase G, A new hydrous magnesium silicate synthesized at 22 GPa and 1050°CGeophysical Research Letters, 1997
- Amorphization of Serpentine at High Pressure and High TemperatureScience, 1996
- Phase F, a new hydrous magnesium silicate synthesized at 1000 °C and 17 GPa: Crystal structure and estimated bulk modulusPhysics and Chemistry of Minerals, 1995
- Thin crust, ultramafic exposures, and rugged faulting patterns at the Mid-Atlantic Ridge (22°–24°N)Geology, 1995
- The role of volatiles in the transition zoneJournal of Geophysical Research, 1993
- Subducting slabs stagnant in the mantle transition zoneJournal of Geophysical Research, 1992
- Relationship of deep seismicity to the thermal structure of subducted lithosphereNature, 1991
- Stability of hydrous magnesium silicates in the mantle transition zonePhysics of the Earth and Planetary Interiors, 1991
- Phase relations in the transition zoneJournal of Geophysical Research, 1990
- The system Mg2SiO4MgOH2O at high pressures and temperatures — Possible hydrous magnesian silicates in the mantle transition zonePhysics of the Earth and Planetary Interiors, 1980