Crustal and upper mantle structure beneath the apennines region as inferred from the study of Rayleigh waves
Item
Title (Dublin Core)
en-US
Crustal and upper mantle structure beneath the apennines region as inferred from the study of Rayleigh waves
Description (Dublin Core)
en-US
Rayleigh wave phase velocities were obtained in the period range 12.5–83.3 s using the almost linear array of long period seismic stations installed at Bari (BAI), Grosseto (GSO), Bologna (BOL), and Torino (TNO). The Hedgehog inversion gives a crustal thickness in the range 25–37 km. The presence of a low-velocity layer in the crust is allowed, while low velocity material within a few kilometers of the Moho is required. The shear-wave velocities below 60 km are rather higher than usual channel values. If crustal thicknesses of the order of 37 km are rejected as suggested by other geophysical data then the low-velocity layer in the crust is required in order to satisfy the observed dispersion relation.
ARK: https://n2t.net/ark:/88439/y089438
Permalink: https://geophysicsjournal.com/article/114
ARK: https://n2t.net/ark:/88439/y089438
Permalink: https://geophysicsjournal.com/article/114
Creator (Dublin Core)
Calcagnile, G.
Panza, G.F.
Subject (Dublin Core)
en-US
Rayleigh waves
en-US
Crust
en-US
Upper mantle
en-US
Italy
en-US
Solid Earth
Publisher (Dublin Core)
en-US
Journal of Geophysics
Date (Dublin Core)
1978-12-22
Type (Dublin Core)
info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
en-US
Peer-reviewed Article
Format (Dublin Core)
application/pdf
Identifier (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/114
Source (Dublin Core)
en-US
Journal of Geophysics; Vol 45 No 1 (1978): Journal of Geophysics; 319-327
2643-2986
2643-9271
Language (Dublin Core)
eng
Relation (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/114/76