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...
Guardado en:
| Autores principales: | Álvarez Pontoriero, Orlando, Giménez, Mario Ernesto, Folguera Telichevsky, Andrés, Guillen, Sofía, Tocho, Claudia Noemí |
|---|---|
| Formato: | Articulo |
| Lenguaje: | Inglés |
| Publicado: |
2018
|
| Materias: | |
| Acceso en línea: | http://sedici.unlp.edu.ar/handle/10915/101268 https://ri.conicet.gov.ar/11336/41366 |
| Aporte de: |
Ejemplares similares
-
Goce derived geoid changes before the Pisagua 2014 earthquake
por: Álvarez, O., et al. -
Goce derived geoid changes before the Pisagua 2014 earthquake
Publicado: (2018) -
Gradients from GOCE reveal gravity changes before Pisagua Mw = 8.2 and Iquique Mw = 7.7 large megathrust earthquakes
por: Folguera, Andrés
Publicado: (2015) -
Gradients from GOCE reveal gravity changes before Pisagua Mw = 8.2 and Iquique Mw = 7.7 large megathrust earthquakes
por: Álvarez, O., et al. -
Static Stress Increase in the Outer Forearc Produced by MW 8.2 September 8, 2017 Mexico Earthquake and its Relation to the Gravity Signal
por: Spagnotto, S., et al.