GOCE derived vertical gravity gradient delineates great earthquake rupture zones along the Chilean margin

In the south Central Andes region, the Nazca oceanic plate that subducts beneath the South American plate is characterized by a rough topography derived from different oceanic features that collide against the continental margin. These features determine an important segmentation of both the margin...

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Detalles Bibliográficos
Autores principales: Álvarez, O., Nacif, S., Gimenez, M., Folguera, A., Braitenberg, C.
Formato: JOUR
Materias:
Earthquake
GOCE
High oceanic features
Rupture zones
Trench sediments
Vertical gravity gradient
Earthquake effects
Earthquakes
Gravitation
Density variations
Gravity gradients
Megathrust earthquakes
Rupture zone
Statistical comparisons
Vertical gradients
Planetary surface analysis
continental margin
earthquake rupture
gravity field
Nazca plate
satellite data
subduction zone
Chile
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00401951_v622_n_p198_Alvarez
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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