Shear-wave Velocity Structure of Greenland from Rayleigh-wave Analysis
The elastic structure beneath Greenland is shown by means of S-velocity maps for depths ranging from zero to 350 km, determined by the regionalization and inversion of Rayleigh-wave dispersion. The traces of 50 earthquakes, occurring from 1990 to 2011, have been used to obtain Rayleigh-wave dispersi...
- Autores:
-
Corchete, V.
- Tipo de recurso:
- Article of journal
- Fecha de publicación:
- 2016
- Institución:
- Universidad Nacional de Colombia
- Repositorio:
- Universidad Nacional de Colombia
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.unal.edu.co:unal/63624
- Acceso en línea:
- https://repositorio.unal.edu.co/handle/unal/63624
http://bdigital.unal.edu.co/64070/
- Palabra clave:
- 55 Ciencias de la tierra / Earth sciences and geology
Rayleigh wave
Shear wave
crust
upper mantle
Greenland
- Rights
- openAccess
- License
- Atribución-NoComercial 4.0 Internacional