1.- ¿PORQUE HAY TERREMOTOS? 2001 Ver registro 2.- 2006 Copiapo Chile seismic swarm analysis; mapping the interplate contact American Geophysical Union; Washington, DC; USA; United States, 2006 AGU 2006 fall meeting Ver registro 3.- 3D geodynamic modeling of slab detachment Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2008 European Geoscience Union general assembly 2008 Ver registro 4.- A KINEMATIC MODEL OF THE SCOTIA PLATE (SW ATLANTIC OCEAN) ELSEVIER; OXFORD; GBR; UNITED KINGDOM, 2003 Ver registro 5.- A Paleo-Mesoproterozoic supercontinent; assembly, growth and breakup Elsevier; Amsterdam; NLD; Netherlands, 2004 Ver registro 6.- A REVIEW OF PLEISTOCENE GIANT ARMADILLOS (MAMMALIA, XENARTHRA, PAMPATHERIIDAE) UNIVERSITY OF TORONTO PRESS; TORONTO, ON; CAN; CANADA, 1996 PALAEOECOLOGY AND PALAEOENVIRONMENTS OF LATE CENOZOIC MAMMALS; TRIBUTES TO THE CAREER OF C. S. (RUFUS) CHURCHER Ver registro 7.- A ZONE OF LITHOSPHERE WEAKNESS BENEATH THE NORTHERN ANDES REVEALED BY FORELAND BASIN GEOMETRY, TOPOGRAPHY AND GRAVITY ANOMALIES AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2000 AGU 2000 FALL MEETING Ver registro 8.- Active faulting and forearc block rotation in south-central Chile from GPS-derived deformation (36-39 degrees S) Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2008 European Geosciences Union general assembly 2008 Ver registro 9.- Active upper plate thrust faulting in regions of low plate interface coupling, repeated slow slip events, and coastal uplift; example from the Hikurangi Margin, New Zealand American Geophysical Union and The Geochemical Society;; USA; United States, 2011 Ver registro 10.- AFRICAN, SOUTHERN INDIAN AND SOUTH AMERICAN CRATONS WERE NOT PART OF THE RODINIA SUPERCONTINENT; EVIDENCE FROM FIELD RELATIONSHIPS AND GEOCHRONOLOGY ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 2003 OROGENIC BELTS, REGIONAL AND GLOBAL TECTONICS; A MEMORIAL VOLUME TO CHRIS MCAULAY POWELL Ver registro
