Registros del 1 al 10 de 10 encontrados |
![](./images/clear.gif) 1.- Aftershock seismicity of the 27 February 2010 Mw 8.8 Maule earthquake rupture zone
Elsevier; Amsterdam; NLD; Netherlands, 2012
Ver registro
![](./images/clear.gif) 2.- Alteration of the subducting oceanic lithosphere at the southern central Chile trench-outer rise
American Geophysical Union and The Geochemical Society;; USA; United States, 2007
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![](./images/clear.gif) 3.- Control of high oceanic features and subduction channel on earthquake ruptures along the Chile-Peru subduction zone
Elsevier; Amsterdam; NLD; Netherlands, 2011
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![](./images/clear.gif) 4.- Effect of trench-outer rise bending-related faulting on seismic Poisson's ratio and mantle anisotropy; a case study offshore of southern central Chile
Blackwell Science for the Royal Astronomical Society, the Deutsche Geophysikalische Gesellschaft and, 2008
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![](./images/clear.gif) 5.- Investigating subduction zone processes in Chile
American Geophysical Union; Washington, DC; USA; United States, 2006
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![](./images/clear.gif) 6.- Revealing the deep structure and rupture plane of the 2010 Maule, Chile earthquake (Mw=8.8) using wide angle seismic data
Elsevier; Amsterdam; NLD; Netherlands, 2011
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![](./images/clear.gif) 7.- Sedimentary fill of the Chile Trench (32-46 degrees S); volumetric distribution and causal factors
Geological Society of London; London; GBR; United Kingdom, 2013
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![](./images/clear.gif) 8.- Structure and local seismicity from the incoming Nazca Plate in the southern Chile subduction zone
American Geophysical Union; Washington, DC; USA; United States, 2005
AGU 2005 fall meeting
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![](./images/clear.gif) 9.- Upper lithospheric structure of the subduction zone offshore of southern Arauco area, Chile ( approximately 38 degrees S)
[International Geological Congress]; [location varies]; III; International, 2008
33rd international geological congress; abstracts
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![](./images/clear.gif) 10.- Upper lithospheric structure of the subduction zone offshore of southern Arauco Peninsula, Chile, at approximately 38 degrees S
American Geophysical Union; Washington, DC; USA; United States, 2008
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