Fast probing of many Earth models with full waveforms
<p>Seismology is our primary method for inferring the structure and dynamics of Earth’s interior. A region of particular importance is the lowermost mantle near the core-mantle boundary. Detailed information about lowermost mantle seismic structures can be inferred by comparing synthetic seism...
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| Format: | Thesis |
| Language: | English |
| Published: |
2019
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