The black lines depict the distribution of major seismogenic faults in the model (after Shen et al., 2004). Red circles mark the locations of earthquakes (M≥6.5) since 1303; white arrows depict displacement directions of the model boundaries. The surface of the model is set free, the bottom horizontally and vertically fixed to velocity zero.</p
International audienceThe geometry of continental fault systems, and more specifically the spatial o...
Abstract—There are currently three major competing views on the essential geometrical, mechanical, a...
We present a seismological technique for determining the down-dip shape of seismogenic normal faults...
A two-dimensional finite element model was constructed along a cross section almost perpendicular to...
Developing 3D representations of active faults is an important step to improve seismic‐hazard assess...
Model A includes models differing in the center distance. Model B includes models differing in the o...
T-axes of the earthquakes analyzed are shown with black arrows. The preferred nodal planes are shown...
A spring mesh model, Spring3D, that simulates the spatial distribution of strain around major faults...
Recent decades have seen dramatic improvement in the ability of earth scientists to resolve the geom...
The characterization of fault zone structure and its evolution is essential for understanding earthq...
No complete physically consistent model of earthquake rupture exists that can fully describe the ric...
[1] We study the distribution of initial stress and frictional parameters for the 28 June 1992 Lande...
The earths crust is constantly in motion. Sections of the crust, called plates, push against each o...
International audienceIn Solid Modeling, a boundary representation (b-rep) defines solids by their b...
<p>The tectonic boundary conditions (black) consist of a 50 mm/yr indentation of a rigid block at th...
International audienceThe geometry of continental fault systems, and more specifically the spatial o...
Abstract—There are currently three major competing views on the essential geometrical, mechanical, a...
We present a seismological technique for determining the down-dip shape of seismogenic normal faults...
A two-dimensional finite element model was constructed along a cross section almost perpendicular to...
Developing 3D representations of active faults is an important step to improve seismic‐hazard assess...
Model A includes models differing in the center distance. Model B includes models differing in the o...
T-axes of the earthquakes analyzed are shown with black arrows. The preferred nodal planes are shown...
A spring mesh model, Spring3D, that simulates the spatial distribution of strain around major faults...
Recent decades have seen dramatic improvement in the ability of earth scientists to resolve the geom...
The characterization of fault zone structure and its evolution is essential for understanding earthq...
No complete physically consistent model of earthquake rupture exists that can fully describe the ric...
[1] We study the distribution of initial stress and frictional parameters for the 28 June 1992 Lande...
The earths crust is constantly in motion. Sections of the crust, called plates, push against each o...
International audienceIn Solid Modeling, a boundary representation (b-rep) defines solids by their b...
<p>The tectonic boundary conditions (black) consist of a 50 mm/yr indentation of a rigid block at th...
International audienceThe geometry of continental fault systems, and more specifically the spatial o...
Abstract—There are currently three major competing views on the essential geometrical, mechanical, a...
We present a seismological technique for determining the down-dip shape of seismogenic normal faults...
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