Change in the pattern of crustal seismicity at the Southern Central Andes from a local seismic network

Shallow seismicity in the Southern Central Andes is associated with interplate earthquakes due to the subduction of the Nazca plate beneath the South American plate and neotectonic activity, mainly located in the retro-arc region. However, this pattern changes drastically south of 34°S within the tr...

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Detalles Bibliográficos
Autores principales:	Nacif, S., Lupari, M., Triep, E.G., Nacif, A., Álvarez, O., Folguera, A., Gímenez, M.
Formato:	JOUR
Materias:	Andean growth Crustal seismicity Erosion Fore-arc and intra-arc and back-arc Southern Central Andes Geophysics Plates (structural components) Seismology Tectonics Back-arc Central Andes Crustal earthquakes Inhomogeneous distribution Interplate earthquakes Precipitation patterns Sub-critical condition Earthquakes backarc basin earthquake event erosion forearc basin Nazca plate neotectonics seismicity subduction zone upper crust Andes Chile
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00401951_v708_n_p56_Nacif
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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