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
Publicado:	2018
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:	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_16749847_v9_n1_p50_Alvarez 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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