Earthquake hypocenters recorded in the Andean Southern Puna seismic array (25–28°S, 70–65°W) provide new constraints on the shape of the subducting Nazca plate beneath the Puna plateau, the transition into the Chilean-Pampean flat slab and the thermal state of the mantle and crust. Some 270 new mantle hypocenters suggest that the subducting slab under the Puna shoals into the flat-slab segment more abruptly and farther to the north than previously indicated. The revised geometry is consistent with the Central Volcanic Zone Incapillo caldera being the southernmost center with Pleistocene activity until reaching the southern side of the flat-slab region. Evidence for the revised slab geometry includes three well-defined hypocenter clusters in...
New fault data and mapping of volcanic rocks from northwestern Argentina's Cordillera de San Buenave...
We have determined the Wadati–Benioff Zone seismicity and state of stress of the subducting Nazca sl...
The subduction zone of central Chile (36°S) has produced some of the world's largest earthquakes and...
A new seismic model for crust and upper mantle of the south Central Andes is derived from full wavef...
The southern Puna Plateau has been proposed to result from a major Pliocene delamination event that ...
A network of 60 seismographs was deployed across the Andes at approximately 23.5°S. The array was ce...
The current western margin of the South American continent is an active subduction orogeny, which is...
An array of 74 seismological stations was deployed in the Argentine Puna and adjacent regions for a...
The western margin of South America between 30ºS and 36ºS is seismically active. While the largest m...
In order to better understand the evolution of continental plateaus in an Andean type plate boundary...
A lingering question in Cordilleran tectonics is how high plateaus form in the absence of continenta...
Shallow seismicity in the Southern Central Andes is associated with interplate earthquakes due to th...
Beneath central Chile and western Argentina, the oceanic Nazca slab drastically changes geometry fro...
The analysis of magmatic distribution, basin formation, tectonic evolution and structural styles of ...
We present a teleseismic P and S receiver function study using data from a temporary passive-source ...
New fault data and mapping of volcanic rocks from northwestern Argentina's Cordillera de San Buenave...
We have determined the Wadati–Benioff Zone seismicity and state of stress of the subducting Nazca sl...
The subduction zone of central Chile (36°S) has produced some of the world's largest earthquakes and...
A new seismic model for crust and upper mantle of the south Central Andes is derived from full wavef...
The southern Puna Plateau has been proposed to result from a major Pliocene delamination event that ...
A network of 60 seismographs was deployed across the Andes at approximately 23.5°S. The array was ce...
The current western margin of the South American continent is an active subduction orogeny, which is...
An array of 74 seismological stations was deployed in the Argentine Puna and adjacent regions for a...
The western margin of South America between 30ºS and 36ºS is seismically active. While the largest m...
In order to better understand the evolution of continental plateaus in an Andean type plate boundary...
A lingering question in Cordilleran tectonics is how high plateaus form in the absence of continenta...
Shallow seismicity in the Southern Central Andes is associated with interplate earthquakes due to th...
Beneath central Chile and western Argentina, the oceanic Nazca slab drastically changes geometry fro...
The analysis of magmatic distribution, basin formation, tectonic evolution and structural styles of ...
We present a teleseismic P and S receiver function study using data from a temporary passive-source ...
New fault data and mapping of volcanic rocks from northwestern Argentina's Cordillera de San Buenave...
We have determined the Wadati–Benioff Zone seismicity and state of stress of the subducting Nazca sl...
The subduction zone of central Chile (36°S) has produced some of the world's largest earthquakes and...