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Are seismic and aseismic slip patches influenced by the late-interseismic physical state of a megathrust? Results from the southern end of the 2010 Maule Chile earthquake

Authors
/persons/resource/marcos

Moreno,  M.
3.1 Lithosphere Dynamics, 3.0 Geodynamics and Geomaterials, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/haber

Haberland,  Christian
2.2 Geophysical Deep Sounding, 2.0 Physics of the Earth, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/oncken

Oncken,  Onno
3.1 Lithosphere Dynamics, 3.0 Geodynamics and Geomaterials, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Rietbrock,  A.
External Organizations;

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Heidbach,  Oliver
2.6 Seismic Hazard and Stress Field, 2.0 Physics of the Earth, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

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Citation

Moreno, M., Haberland, C., Oncken, O., Rietbrock, A., Heidbach, O. (2012): Are seismic and aseismic slip patches influenced by the late-interseismic physical state of a megathrust? Results from the southern end of the 2010 Maule Chile earthquake, (Geophysical Research Abstracts Vol. 14, EGU2012-8185-1, 2012), General Assembly European Geosciences Union (Vienna, Austria 2012).


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_246997
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