P- waves reflected from the "20" discontinuity" beneath the Mediterranean region

The observed travel-times of the P-waves for twenty
 shallow, intermediate, and deep earthquakes, with epicenters in the Mediterranean
 area, are used in order to analyze some characteristics of the
 upper mantle.
 A first- order discontinuity, identifiable as the &qu...

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Bibliographic Details
Main Authors: B. FEDERICO, A BOTTARI
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1975-05-01
Series:Annals of Geophysics
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/4892