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...
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Format: | Article in Journal/Newspaper |
Language: | Spanish |
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Universidad Nacional de Colombia - Sede Bogotá - Facultad de Ciencias - Departamento de Geociencia
2016
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Online Access: | https://repositorio.unal.edu.co/handle/unal/63624 http://bdigital.unal.edu.co/64070/ |