The eastern Sierras Pampeanas (ESP) are the easternmost expression of a series of foreland uplifts in the Argentine back arc region (similar to 30-34 degrees S) and show spatial and temporal connections with the subduction of the Juan Fernandez Ridge (JFR) under the South American plate. In order to get new insights on the mechanisms that control crustal regional tectonics, we computed teleseismic receiver functions (RF) and jointly invert them with Rayleigh-wave phase velocity dispersion curves. RR allow resolving crustal thickness and infra crustal velocity variations with a good vertical resolution whereas surface wave information helps to constrain absolute seismic wave velocities. Our seismic images have been combined with crustal ...
The subduction of the Nazca plate under the South American plate around 31°S is characterized by fla...
In this study, we analyze 100 crustal Precordilleran earthquakes recorded in 2008 and 2009 by 52 bro...
A digitally recording seismic network was operated from September 1987 to May 1988 in the San Juan P...
The eastern Sierras Pampeanas (ESP) are the easternmost expression of a series of foreland uplifts i...
The Pampean flat slab of central Chile and Argentina (30◦–32◦S) has strongly influenced Cenozoic tec...
Local network data from San Juan, Argentina, provides new information about crustal seismicity in th...
The Eastern Sierras Pampeanas located \u3e600 km east of the Andean Cordillera is interpreted to be ...
The Nazca Plate subducting beneath the South American Plate, has strongly influenced Cenozoic-mounta...
We obtain earthquake locations and a detailed three-dimensional velocity model of the flat slab subd...
The western margin of South America between 30ºS and 36ºS is seismically active. While the largest m...
In the flat slab region of the South Central Andes (∼31–32◦S), geological observations suggest that ...
In the central Andes, the Nazca plate displays large along strike variations in dip with a near hori...
Abstract Local network three-component digital data from the San Juan area, Argentina, provide the f...
A new seismic model for crust and upper mantle of the south Central Andes is derived from full wavef...
A local seismic network, operating in western Argentina from 28°S to 33 °S, between August 1995 and...
The subduction of the Nazca plate under the South American plate around 31°S is characterized by fla...
In this study, we analyze 100 crustal Precordilleran earthquakes recorded in 2008 and 2009 by 52 bro...
A digitally recording seismic network was operated from September 1987 to May 1988 in the San Juan P...
The eastern Sierras Pampeanas (ESP) are the easternmost expression of a series of foreland uplifts i...
The Pampean flat slab of central Chile and Argentina (30◦–32◦S) has strongly influenced Cenozoic tec...
Local network data from San Juan, Argentina, provides new information about crustal seismicity in th...
The Eastern Sierras Pampeanas located \u3e600 km east of the Andean Cordillera is interpreted to be ...
The Nazca Plate subducting beneath the South American Plate, has strongly influenced Cenozoic-mounta...
We obtain earthquake locations and a detailed three-dimensional velocity model of the flat slab subd...
The western margin of South America between 30ºS and 36ºS is seismically active. While the largest m...
In the flat slab region of the South Central Andes (∼31–32◦S), geological observations suggest that ...
In the central Andes, the Nazca plate displays large along strike variations in dip with a near hori...
Abstract Local network three-component digital data from the San Juan area, Argentina, provide the f...
A new seismic model for crust and upper mantle of the south Central Andes is derived from full wavef...
A local seismic network, operating in western Argentina from 28°S to 33 °S, between August 1995 and...
The subduction of the Nazca plate under the South American plate around 31°S is characterized by fla...
In this study, we analyze 100 crustal Precordilleran earthquakes recorded in 2008 and 2009 by 52 bro...
A digitally recording seismic network was operated from September 1987 to May 1988 in the San Juan P...