Comparative analysis of Pn full-waveform inversion and travel-time tomography in imaging upper mantle azimuthal anisotropy
Conventional Pn-wave imaging techniques, typically based on the ray theory, rely on Pn travel times to resolve the 2-D velocity and azimuthal anisotropy structures of the uppermost mantle. However, these approaches neglect the finite-frequency effects of wave propagation, thereby being limited in re...
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| Hlavní autoři: | , , , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
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Frontiers Media S.A.
2026-02-01
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| Edice: | Frontiers in Earth Science |
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| On-line přístup: | https://www.frontiersin.org/articles/10.3389/feart.2026.1748581/full |
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