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Hauke Marquardt is a professor in the Department of Earth Sciences at the University of Oxford, where he employs state-of-the-art experimental techniques to understand properties of materials under extreme pressure and temperature conditions typical of the deep interiors of planets. His research incorporates high-level processes occurring in planetary systems and focuses on four main directions: developing Deep Earth Mantle Phase Transition Maps, exploring the structure and composition of rocky planets, understanding dynamics of planetary interiors through dynamic compression experiments, and investigating planetary ice compounds to improve models of ice giants like Mini-Neptune. Marquardt's work utilizes advanced methods such as x-ray diffraction and optical spectroscopy, among others, to analyze materials and create large-scale dynamic models that simulate planetary evolution over time. This research is critical in interpreting planetary observations and leveraging empirical data to enhance our understanding of geochemical variabilities across different celestial bodies.
University of Oxford • Oxford, UK
Professor in the Department of Earth Sciences.
University of Oxford • Oxford, UK
Associate Professor of Solid Earth Geosciences.
Worcester College, Oxford • Oxford, UK
Member of the governing body, involved in academic tutoring.
Bayerisches Geoinstitut (BGI), University of Bayreuth • Bayreuth, Germany
Led a group focusing on geosciences research.
German Research Center for Geosciences (GFZ), Potsdam • Potsdam, Germany
Conducted postdoctoral research in geosciences.
University of California, Berkeley • Berkeley, CA, USA
Postdoctoral position focused on planetary geosciences.
Department of Politics and International Relations - Higher Level English requirement.