Structure of the seismogenic zone of the southcentral Chilean margin revealed by local earthquake traveltime tomography

Author:

Haberland Christian12,Rietbrock Andreas3,Lange Dietrich245,Bataille Klaus6,Dahm Torsten4

Affiliation:

1. Deutsches GeoForschungsZentrum; Potsdam Germany

2. Institute of Geosciences; University of Potsdam; Potsdam Germany

3. Department of Earth and Ocean Sciences; University of Liverpool; Liverpool UK

4. Institute of Geophysics; University of Hamburg; Hamburg Germany

5. Bullard Laboratories; University of Cambridge; Cambridge UK

6. Departamento Ciencias De La Tierra; Universidad de Concepción; Concepción Chile

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference99 articles.

1. Hydrated subducted crust at 100-250 km depth;Abers;Earth Planet. Sci. Lett.,2000

2. Distribution of metamorphic facies in Chile - an outline;Aguirre;Krystallinikum,1972

3. Angermann , D. G. Baustert R. Galas S. Y. Zhu 1997 EPOS. P.V3 (Earth Parameter and Orbit System): Software user manual for GPS data processing Sci. Tech. Rep. STR 97/14 GeoForschungsZentrum Potsdam, Germany

4. Episodic development of a convergent margin inferred from structures and processes along the southern Chile margin;Bangs;Tectonics,1997

5. The 1960 Chile earthquake: Inversion for slip distribution from surface deformation;Barrientos;Geophys. J. Int.,1990

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