Stanford Doerr School of Sustainability
Showing 31-40 of 142 Results
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Anton Ermakov
Assistant Professor of Aeronautics and Astronautics and, by courtesy, of Geophysics and of Earth and Planetary Sciences
Current Research and Scholarly InterestsI am interested in the formation and evolution of the Solar System bodies and the ways we can constrain planetary interiors by geophysical measurements.
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W Gary Ernst
The Benjamin M. Page Professor in Earth Sciences, Emeritus
Current Research and Scholarly InterestsPetrology/geochemistry and plate tectonics of Circumpacific and Alpine mobile belts; ultrahigh-pressure metamorphism in Eurasia; geology of the California Coast Ranges, the cental Klamath Mountains, and White-Inyo Range; geobotany and remote sensing of the American Southwest; mineralogy and human health.
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Amir Eskanlou
Postdoctoral Scholar, Earth and Planetary Sciences
BioAmir is a postdoctoral scholar at Stanford Mineral-X. With 15 years of research and industry experience, his background includes the development and optimization of mineral processing flowsheets for copper, phosphate, graphite and rare earth elements (REEs) from primary and secondary resources. At Stanford, he conducts research related to various aspects of critical minerals processing, including AI-driven reagent discovery, uncertainty quantification, circuit design, and optimization of energy and water consumption.
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Stephan Graham
Welton Joseph and Maud L'Anphere Crook Professor of Applied Earth Sciences & by courtesy, of Geophysics & of Energy Science Engineering
Current Research and Scholarly InterestsSedimentary basin analysis; petroleum geology
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Martin Grove
Professor (Research) of Earth and Planetary Sciences
Current Research and Scholarly InterestsResearch
I study the evolution of the Earth's crust by undertaking petrologic and geochemically-based research that is grounded with fieldwork. I co-direct the Stanford-USGS ion probe laboratory and develop geochronologic methods to constrain crystallization, metamorphic, and metasomatic histories of the middle to deep crust. Similarly, because heat flow characteristically attends mass transfer during crustal deformation, I employ 40Ar/39Ar and (U-Th)/He thermochronology to extract thermal history information from minerals to constrain the timing and magnitude of fault slip as well as erosional and tectonic denudation. Finally, I am heavily involved in provenance studies to constrain aspects of crustal deformation and erosion that are only preserved in the sedimentary record.
