His scientific interests lie mostly in Scaling, Anisotropy, Geophysics, Sea ice and Seismology. His Scaling research incorporates elements of Strike-slip tectonics, Perpendicular, Optics and Scale invariance. The study incorporates disciplines such as Lidar and Active fault in addition to Anisotropy.
His Sea ice research is classified as research in Climatology. Seismology is a component of his Remotely triggered earthquakes, Aftershock, Earthquake swarm, Plate tectonics and Structural geology studies. David Marsan performs multidisciplinary studies into Aftershock and Cascade in his work.
His primary scientific interests are in Seismology, Induced seismicity, Aftershock, Sea ice and Geophysics. His Induced seismicity study combines topics in areas such as Epicenter, Tectonics, North Anatolian Fault and Crust. His Aftershock research also works with subjects such as
In his research on the topic of Sea ice, Buoy is strongly related with Arctic. In his research, Anisotropy, Predictability, Deformation and Scale invariance is intimately related to Scaling, which falls under the overarching field of Geophysics. His Sea ice thickness course of study focuses on Drift ice and Antarctic sea ice.
Seismology, Induced seismicity, Foreshock, Aftershock and Tectonophysics are his primary areas of study. He combines Seismology and Nucleation in his studies. His Induced seismicity research includes elements of Inverse and Fault gouge.
His studies in Foreshock integrate themes in fields like Earthquake catalog and Earthquake detection. His research integrates issues of Statistical physics, Stress drop and Scaling in his study of Aftershock. The various areas that David Marsan examines in his Tectonophysics study include Intraplate earthquake and Deformation.
David Marsan spends much of his time researching Seismology, Induced seismicity, Nucleation, Subduction and Scaling. His work deals with themes such as Fault slip, Aftershock, San andreas fault, Coincident and Stress drop, which intersect with Scaling. David Marsan combines Stress drop and Broad spectrum in his research.
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Extending Earthquakes' Reach Through Cascading
David Marsan;Olivier Lengliné.
Science (2008)
Multifractal Cascade Dynamics and Turbulent Intermittency
D. Schertzer;S. Lovejoy;F. Schmitt;Y. Chigirinskaya.
Fractals (1997)
Positive trend in the mean speed and deformation rate of Arctic sea ice, 1979–2007
P. Rampal.;P. Rampal.;Jérôme Weiss;D. Marsan.
Journal of Geophysical Research (2009)
Characterization of Fault Roughness at Various Scales: Implications of Three-Dimensional High Resolution Topography Measurements
Thibault Candela;François Renard;Michel Bouchon;Alexandre Brouste.
Pure and Applied Geophysics (2009)
The long precursory phase of most large interplate earthquakes
Michel Bouchon;Virginie Durand;Virginie Durand;David Marsan;Hayrullah Karabulut.
Nature Geoscience (2013)
Three-Dimensional Mapping of Dislocation Avalanches: Clustering and Space/Time Coupling
Jérôme Weiss;David Marsan.
Science (2003)
Causal space‐time multifractal processes: Predictability and forecasting of rain fields
David Marsan;Daniel Schertzer;Shaun Lovejoy.
Journal of Geophysical Research (1996)
High resolution 3D laser scanner measurements of a strike-slip fault quantify its morphological anisotropy at all scales
François Renard;François Renard;Christophe Voisin;David Marsan;Jean Schmittbuhl.
Geophysical Research Letters (2006)
Characterization of Fault Roughness at Various Scales: Implications of Three-Dimensional High Resolution Topography Measurements
Thibault Candela;François Renard;Michel Bouchon;David Marsan.
arXiv: Geophysics (2008)
Scale dependence and localization of the deformation of Arctic sea ice.
David Marsan;Harry Stern;Ron Lindsay;Jérôme Weiss.
Physical Review Letters (2004)
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