Physics
Scientist
Faculty of Geosciences, Utrecht University, Utrecht, Netherlands
Department of Earth Sciences, Utrecht University, Utrecht 3584 CD, The Netherlands
Utrecht University, Department of Earth Sciences, Seismology, Budapestlaan 4, 3584 CD Utrecht, The Netherlands
Department of Earth Sciences, Utrecht University, PO Box 80021, 3508 TA Utrecht, the Netherlands. of Geophysics, Utrecht University, Budapestlaan 4, P.O. Box 80021, 3508 TA, Utrecht, The Netherlands
Department of Geophysics, Utrecht University, P.O. Box 80021, TA 3058, Utrecht, The Netherlands
Department of Earth Sciences, Utrecht University, PO Box 80021, Utrecht 3584 CD, The Netherlands. of Earth Sciences, Utrecht University, Utrecht 3584 CD, The Netherlands. of Earth Sciences, University of Utrecht, Budapestlaan 4, 3584 CD, Utrecht, The Netherlands
Department of Earth Sciences, Utrecht University, Utrecht, Netherlands
Faculty of Earth Sciences, Utrecht University, Utrecht, the Netherlands.
Department of Earth Sciences, Utrecht University, Utrecht, The Netherlands
Department of Geophysics, Utrecht University, PO BOX 80021, 3508 TA Utrecht, the Netherlands
Faculty of Earth Sciences, Utrecht University, Utrecht, The Netherlands
Department of Geophysics, Utrecht University, PO Box 80.021, 3508 TA Utrecht, the Netherlands. URA 1358-Ecole et Observatoire de Physique du Globe, 5 Rue René Descartes, 67084 Strasbourg Cedex, France
Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, the Netherlands.
Utrecht University, Department of Earth Sciences, Budapestlaan 4, 3584 CD Utrecht, the Netherlands. of Earth Sciences, Utrecht University, Post Office Box 80021, 3508 TA Utrecht, Netherlands.
Department of Earth Sciences, Utrecht University, PO Box 80021, TA 3058 Utrecht, the Netherlands.
A comparison between lower mantle models from probabilistic tomography and models of thermo-chemical convection
Anomalies of temperature and iron in the uppermost mantle inferred from gravity data and tomographic models
Approximations in seismic interferometry and their effects on surface waves
Are we exceeding the limits of the great circle approximation in global surface wave tomography?
Assessment of global phase velocity models
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