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Predictions and Observations for the Oceanic Lithosphere From S‐to‐P Receiver Functions and SS Precursors
The ocean lithosphere is classically described by the thermal half‐space cooling (HSC) or the plate models, both characterized by a gradual transition to the asthenosphere beneath. Scattered waves find sharp seismic discontinuities beneath the oceans, possibly from the base of the plate. Active sour...
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| Publicado no: | Geophys Res Lett |
|---|---|
| Main Authors: | , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
John Wiley and Sons Inc.
2018
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6049891/ https://ncbi.nlm.nih.gov/pubmed/30034045 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1029/2018GL077675 |
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