SUL GRADIENTE DI TEMPERATURA NECESSARIO per la FORMAZIONE DI LOW-VELOCITY LAYERS
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Abstract
È noto che se la velocità delle onde sismiche, a partire
da una certa profondità, diminuisce raggiungendo un minimo e
poi cresce nuovamente, si forma un « low-velocity layer » o strato di
bassa velocità.
da una certa profondità, diminuisce raggiungendo un minimo e
poi cresce nuovamente, si forma un « low-velocity layer » o strato di
bassa velocità.
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How to Cite
(1)
VALLE, P. E. SUL GRADIENTE DI TEMPERATURA NECESSARIO Per La FORMAZIONE DI LOW-VELOCITY LAYERS. Ann. Geophys. 1956, 9 (3), 371-377. https://doi.org/10.4401/ag-5612.
