TEM observations of several spinel‐garnet assemblies: toward the rheology of the transition zone
- 1 September 1995
- journal article
- Published by Wiley in Terra Nova
- Vol. 7 (5) , 509-515
- https://doi.org/10.1111/j.1365-3121.1995.tb00552.x
Abstract
No abstract availableKeywords
This publication has 27 references indexed in Scilit:
- Plastic deformation of garnets: systematics and implications for the rheology of the mantle transition zoneEarth and Planetary Science Letters, 1995
- Elastic wave velocities of a pyrope-majorite garnet to 3 GPaPhysics of the Earth and Planetary Interiors, 1994
- Layered rheological structure of subducting oceanic lithosphereEarth and Planetary Science Letters, 1994
- Ultradeep, ultramafic mantle xenoliths: transmission electron microscopy preliminary resultsPhysics of the Earth and Planetary Interiors, 1994
- A Griggs deformation apparatus set up at LilleTerra Nova, 1991
- The strength of mantle silicates at high pressures and room temperature: implications for the viscosity of the mantleNature, 1990
- Plasticity-crystal structure systematics in dense oxides and its implications for the creep strength of the Earth's deep interior: a preliminary resultPhysics of the Earth and Planetary Interiors, 1989
- Phase transitions and mantle discontinuitiesReviews of Geophysics, 1983
- Plastic deformation of MgO : n Al2O3 spinels at temperatures below 1000 °C (0.5 Tm)Le Journal de Physique Colloques, 1980
- Dislocations in Spinel and Garnet High-Pressure Polymorphs of Olivine and Pyroxene: Implications for Mantle RheologyScience, 1980