Goce derived geoid changes before the Pisagua 2014 earthquake

The analysis of space – time surface deformation during earthquakes reveals the variable state of stress that occurs at deep crustal levels, and this information can be used to better understand the seismic cycle. Understanding the possible mechanisms that produce earthquake precursors is a key issu...

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Detalles Bibliográficos
Autores principales: Álvarez, O., Gimenez, M., Folguera, A., Guillen, S., Tocho, C.
Formato: JOUR
Materias:
Forecasting and monitoring
Great megathrust earthquakes
Pre-seismic geoid changes
Satellite gravimetry
Subduction zones
coseismic process
crustal structure
deformation
earthquake event
earthquake mechanism
earthquake precursor
earthquake prediction
EOS
geoid
GOCE
gravimetry
intraplate process
monitoring
postseismic process
satellite data
satellite imagery
seismic hazard
seismology
spatiotemporal analysis
subduction zone
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_16749847_v9_n1_p50_Alvarez
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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