Physics
Scientist
Department of Earth and Environmental Sciences, Geophysics Section, Ludwig-Maximilian University, Munich, Germany
Department of Earth and Environmental Sciences, Ludwig-Maximilians-Universität, München, Germany of Theoretical Geophysics, Cambridge, UK
Department of Earth and Environmental Sciences, Ludwig-Maximilians-University of Munich, Munich, Germany
Department of Earth and Environmental Sciences, Ludwig Maximilians Universität, Theresienstrasse 41, 80333 Munich, Germany
Department of Earth and Environmental Sciences, Ludwig Maximilian University, Theresienstrasse 41, 80333 Munich, Germany
Department of Earth and Environmental Sciences, Ludwig-Maximilians-University Munich, Munich, Germany
Institut für Geophysik, Ludwig-Maximilians-Universität München, Munich, Germany
Department of Earth and Environmental Studies, Section Geophysics, Ludwig-Maximilians-University München, Germany
Department of Earth and Environmental Sciences, Ludwig Maximilians Universität, Theresienstrasse 41, 80333 Munich, Germany of Earth and Environmental Sciences, Ludwig-Maximilians-University Munich, Theresienstrasse 41, D-80333 Munich, Germany of Earth and Environmental Sciences, Geophysics Section, Ludwig-Maximilians-Universität, München, Germany
Institute of Theoretical Geophysics, Department of Earth Sciences, Cambridge, CB2 3EQ, UK.
Department of Earth and Environmental Sciences, Ludwig-Maximilians-University of Munich, Theresienstrasse 41, D-80333 Munich, Germany Geophysik, Department für Geo- und Umweltwissenschaften, Ludwig-Maximillians-Universität München, Munich, Germany
Department of Earth and Environmental Sciences, Ludwig-Maximilians-University, Munich,
Acoustic simulation of P-wave propagation in a heterogeneous spherical earth: numerical method and application to precursor waves to PKPdf
An arbitrary high-order Discontinuous Galerkin method for elastic waves on unstructured meshes - III. Viscoelastic attenuation
An arbitrary high-order discontinuous Galerkin method for elastic waves on unstructured meshes ? IV. Anisotropy
Basin-related effects on ground motion for earthquake scenarios in the Lower Rhine Embayment
Broad-band observations of earthquake-induced rotational ground motions
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