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...
שמור ב:
| מחבר ראשי: | |
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| פורמט: | Artigo |
| שפה: | Inglês |
| יצא לאור: |
MDPI AG
2025-04-01
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| סדרה: | Applied Sciences |
| נושאים: | |
| גישה מקוונת: | https://www.mdpi.com/2076-3417/15/9/4732 |
| תגים: |
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