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...
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| Formatua: | Artigo |
| Hizkuntza: | Inglês |
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MDPI AG
2025-04-01
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| Saila: | Applied Sciences |
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| Sarrera elektronikoa: | https://www.mdpi.com/2076-3417/15/9/4732 |
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