The asthenosphere low-velocity layer
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Abstract
Bisultati basati su osservazioni di vari fenomeni provano praticamentel'esistenza di un canale astenosferico a flessione di velocità, diffuso in tuttala terra. L'unione di dati passati e recenti nella velocità dell'onda sismicamostra che sotto i continenti il canale comincia alla discontinuità di Moho. GUTENBERGrovicic, con velocità che sono tanto più piccole quanto più grande è la profonditàdella discontinuità.
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How to Cite
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Gutenberg, B. The Asthenosphere Low-Velocity Layer. Ann. Geophys. 1959, 12 (4), 439-460. https://doi.org/10.4401/ag-5730.