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Institute of Geophysics and Planetary Physics, University of California, Riverside, CA 92521, USA; Department of Earth Sciences, University of California, Riverside, CA 92521, USA
Institute of Geophysics and Planetary Physics, University California, Riverside, USA
Department of Earth Sciences, University of California at Riverside, CA 92521-0412, United States
Department of Earth Sciences, University of California, Riverside, CA 92521, USA; Institute of Geophysics and Planetary Physics, University of California, Riverside, CA 92521, USA
Department of Earth Sciences, University of California at Riverside, Riverside, CA 92521, USA; Institute of Geophysics and Planetary Physics, University California, Riverside, CA 92521, USA
Department of Earth Sciences and Institute of Geophysics and Planetary Physics, University of California, Riverside, CA 92521, USA
Department of Geology, University of California, Davis, CA 95616 USA
Department of Earth Sciences, University of California at Riverside, 92521, Riverside, CA, USA
Institute of Geophysics and Planetary Physics and Department of Earth Sciences, University of California, Riverside, CA 92521, USA
Institute of Geophysics and Planetary Physics, University of California, Riverside, Riverside, CA 92521, USA of Earth Sciences, University of California, Riverside, CA 92521, USA
University of California, Davis, CA 95616 USA
Department of Physics, Florida State University, Tallahassee, FL 32306-4350.
A general test of the hypothesis that transformation-induced faulting cannot occur in the lower mantle
Ca-Eskola component in clinopyroxene: Experimental studies at high pressures and high temperatures in multianvil apparatus
Can Nitrogen be a Candidate for the Fe-Core Formation?
Deformation of peridotite at high pressure in a new molten salt cell: comparison of traditional and homologous temperature treatments
Diamond and Coesite After Former Stishovite in Tibet Ophiolites: Is That Myth or Reality?
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