Statistics – Computation
Scientist
Statistics
Computation
Scientist
ETH Zürich, Zürich, Switzerland
Geophysical Fluid Dynamics, ETH Zürich, Zürich, Switzerland; Geological Faculty, Moscow State University, Moscow, Russia
Institut für Geologie, Mineralogie und Geophysik, Ruhr-Universitt Bochum, 44780 Bochum, Germany; Institute of Experimental Mineralogy Russian Academy of Sciences, 142432 Chernogolovka, Moscow, Russia
Geophysical Fluid Dynamics Group, Institute of Geophysics, Department of Geosciences, ETH-Zurich, Switzerland
Geologisches Institut, ETH, Zürich, CH-8092 Zürich, Switzerland; Institute of Experimental Mineralogy, Russian Academy of Sciences, 142432 Chernogolovka, Moscow, Russia of Geophysics, ETH Zürich, 8092 Zürich, Switzerland
Institut für Geologie, Mineralogie und Geophysik, Ruhr-Universität Bochum, 44780, Bochum, Germany
Geophysical Fluid Dynamics Group, Institute of Geophysics, Department of Geosciences, ETH-Zürich, Switzerland
Institute of Geophysics, ETH Zentrum, 8092, Zürich, Switzerland; Adjunct Professor of Geology Department, Moscow State University, 119899 Moscow, Russia
Swiss Federal Institute of Technology, Department of Geosciences, Zürich, 49802 Switzerland of Geophysics, ETH-Zürich, 8092 Zürich, Switzerland
ETH Zurich, Institute of Geophysics, Geophysical Fluid Dynamics, Sonneggstrasse 5, 8092 Zurich, Switzerland
ETH Zürich, Institute of Geophysics, Zürich, Switzerland
ETH Zürich, Geophysics, Zürich, Switzerland
Geophysical Fluid Dynamics Group, Institute of Geophysics, Department of Geosciences, ETH-Zürich, HPP L.8, Hoenggerberg, Zürich, 8093, Switzerland of Geophysics, ETH Zurich, Switzerland
Institute of Geophysics, ETH-Zürich, 8092 Zürich, Switzerland; Geology Department, Moscow State University, 119899 Moscow, Russia
Institute of Geophysics, Geophysical Fluid Dynamics, ETH Zürich, Schafmattstrasse 30, CH-8093 Zurich, Switzerland.
A comparison of numerical surface topography calculations in geodynamic modelling: an evaluation of the 'sticky air' method
A free plate surface and weak oceanic crust produce single-sided subduction on Earth
Asthenospheric upwelling, oceanic slab retreat, and exhumation of UHP mantle rocks: Insights from Greater Antilles
Characteristics-based marker-in-cell method with conservative finite-differences schemes for modeling geological flows with strongly variable transport properties
Core and early crust formation on Mars
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