Crust and Upper Mantle Structure of Mars Determined from Surface Wave Analysis
The crust and upper mantle structure of Mars is determined in the depth range of 0 to 100 km, by means of dispersion analysis and its inversion, which is performed for the surface waves present in the traces of the seismic event: S1094b. From these traces, Love and Rayleigh waves are measured in the...
Αποθηκεύτηκε σε:
| Κύριος συγγραφέας: | |
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| Μορφή: | Artigo |
| Γλώσσα: | Inglês |
| Έκδοση: |
MDPI AG
2025-04-01
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| Σειρά: | Applied Sciences |
| Θέματα: | |
| Διαθέσιμο Online: | https://www.mdpi.com/2076-3417/15/9/4732 |
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