Pn wave tomography in Greece
In this study, we use Pn seismic wave arrivals to obtain structural information for the upper mantle, lower crust i.e. the Moho discontinuity, in Greece. Previous studies indicate that crustal thickness varies significantly across Greece. In detail, crust has the largest thickness in the Hellenides...
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| Μορφή: | Thesis |
| Γλώσσα: | English |
| Έκδοση: |
2018
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| Διαθέσιμο Online: | http://hdl.handle.net/10889/11047 |
