Statistics – Computation
Scientist
Statistics
Computation
Scientist
Department of Geophysics, Faculty of Mathematics and Physics, Charles University, V Holesovickach 2, PRAGUE, 180 00 Czech Republic
Department of Geophysics, Charles University, Prague, Czech Republic;
Department of Geophysics, Faculty of Mathematics and Physics, Charles University, V Holešovičkách 2, 180 00 Praha 8, Czechoslovakia
CHARLES UNIVERSITY, KG MFF UK, V Holesovickach 2, 180 00, PRAHA, 18000 Czech Republic
Charles University, KG MFF UK, V Holesovickach 2, Prague, 180 00 Czech Republic
Department of Geophysics, Faculty of Mathematics and Physics, Charles University, Prague, Czech Republic
Department of Geophysics, Faculty of Mathematics and Physics, Charles University, V Holešovičkách 2, 18000 Prague, Czech Republic.
Charles Univ., Czech Republic
Department of Geophysics, Faculty of Mathematic and Physics, Charles University, Prague, Czech Republic
Charles University, Department of Geophysics, Prague, 180 00, Czech Republic
Charles University, Department of Geophysics, Faculty of Mathematics and Physics, Charles University, V Holesovickach 2, Prague, 180 00, Czech Republic
Department of Geophysics, Charles University in Prague, Praha, Czech Republic
Department of Geophysics, Charles University, Prague, Czech Republic
Charles University, Department of Geophysics, Prague, Czech Republic
Department of Geophysics, Charles University in Prague, Czech Republic
Charles University, Department of Geophysics, Czech Republic
Charles Univ., Prague, Czech Republic
Department of Geophysics, Faculty of Mathematics and Physics, Charles University, V Holesovickach 2, 180 00 Prague 8, Czech Republic
Department of Geology and Geophysics and Minnesota Supercomputer Institute,
Can long-wavelength dynamical signatures be compatible with layered mantle convection?
Can long-wavelength dynamical signatures be compatible with layered mantle convection?
Can lower mantle slab-like seismic anomalies be explained by thermal coupling between the upper and lower mantles?
Can the 1D viscosity profiles inferred from postglacial rebound data be affected by lateral viscosity variations in the tectosphere?
Comparison between Newtonian and non-Newtonian flow driven by internal loads.
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