On the data integration of seismological observation and deep seismic exploration. The crustal modeling for the Messina Straits Area as an example
Given an earth crust model having homogeneous layers and spherical<br />symmetry, the travel-times equations of the direct and refracted longitudinal<br />waves are first deduced. These linear equations are determined<br />from the seismic ray parameter p, a...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
1981-06-01
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| Series: | Annals of Geophysics |
| Online Access: | http://www.annalsofgeophysics.eu/index.php/annals/article/view/4689 |