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...

Full description

Saved in:
Bibliographic Details
Main Author: V. Corchete
Format: Article
Language:English
Published: Universidad Nacional de Colombia 2016-01-01
Series:Earth Sciences Research Journal
Subjects:
Online Access:https://revistas.unal.edu.co/index.php/esrj/article/view/41079
Tags: Add Tag
No Tags, Be the first to tag this record!