SOME CONSEQUENCE OF THE EXISTENCE OF LOW-VELOCITY LAYERS
The velocities of elastic waves (P and S) generally increase with<br />depth in the earth. If at some depth this increase is replaced by a decrease<br />over an interval of depth, again followed by an increase at some<br />greater depth, we have, what we cal...
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| Format: | Article |
| Language: | English |
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Istituto Nazionale di Geofisica e Vulcanologia (INGV)
1956-06-01
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| Series: | Annals of Geophysics |
| Online Access: | http://www.annalsofgeophysics.eu/index.php/annals/article/view/5615 |