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Scientist
Department of Geological Sciences, Arizona State University, Tempe, AZ 85287-1404, USA
Arizona State University, Department of Geological Sciences, Tempe, AZ 85287, USA
School of Earth and Space Exploration, Arizona State University, Tempe 85287, AZ, USA;
School of Earth & Space Expl., Arizona State University, Tempe 85287, AZ, USA;
School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287, USA
School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287-1404, USA
Planetary Chemistry Laboratory, Department of Earth and PlanetarySciences, Washington University, One Brookings Drive, St Louis, USA
Department of Geological Sciences, Arizona State University, Tempe, AZ 85287, USA
School of Earth and Space Exploration, Arizona State University, P.O. Box 871404, Tempe, AZ 85287-1404, USA
School of Earth & Space Exploraton, Arizona State University, Tempe, AZ, USA
School of Earth and Space Exploration, Arizona State University, Tempe, AZ, USA
VERNADSKY INST. OF GEOCHEMISTRY & ANALYTICAL CHEMISTRY, ACADEMY OF SCIENCES, MOSCOW, USSR
Washington University
Russian Academy of Sciences, Inst. of Geochemistry and Analytical Chemistry, Moscow, Russia
Russian Academy of Sciences, Inst. of Geochemistry and Analytical Chemistry
Department of Geological Sciences, Arizona State University, Box 871404, Tempe, AZ 85287-1404, USA
VERNADSKY INSTITUTE OF GEOCHEMISTRY & ANALYTICAL CHEMISTRY, USSR ACADEMY OF SCIENCES, MOSCOW
VERNADSKY INST. OF GEOCHEMISTRY & ANALYTICAL CHEMISTRY, USSR ACADEMY OF SCIENCE, MOSCOW
School of Earth and Space Exploration, Arizona State University, Tempe, Arizona, USA
Department of Geological Sciences,
A Hydrothermal Origin for the Sulfate-rich Ocean of Europa
A model for low-temperature biogeochemistry of sulfur, carbon, and iron on Europa
A Model of the Physico-Chemical Evolution of the Venus Atmosphere as a Result of Volcanic CO2 Degassing
A Model of the Venus Atmosphere Evolution Along with Titanhematite-Magnetite-Pyrite Buffer
A thermodynamic assessment of the potential synthesis of condensed hydrocarbons during cooling and dilution of volcanic gases
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