Mapping Moho depth variations in central Italy from PsMoho‐P delay times: Evidence of an E‐W transition in the Adriatic Moho at 42°N latitude
Along the Italian peninsula adjoin two crustal domains, peri‐Tyrrhenian and Adriatic, whose boundary is not univocal in central Italy. In this area, we attempt to map the extent of the Moho in the two terrains from variations of the travel time difference between the direct P wave and the P‐to‐S wav...
Wedi'i Gadw mewn:
| Prif Awduron: | , , |
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| Fformat: | Artigo |
| Iaith: | Inglês |
| Cyhoeddwyd: |
Wiley
2013-10-01
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| Cyfres: | Geochemistry, Geophysics, Geosystems |
| Pynciau: | |
| Mynediad Ar-lein: | https://doi.org/10.1002/ggge.20235 |
| Tagiau: |
Dim Tagiau, Byddwch y cyntaf i dagio'r cofnod hwn!
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