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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...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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John Wiley and Sons Inc.
2018
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6049891/ https://www.ncbi.nlm.nih.gov/pubmed/30034045 http://dx.doi.org/10.1029/2018GL077675 |