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...
| Veröffentlicht in: | Geophysical research letters. - 1984. - 45(2018), 11 vom: 16. Juni, Seite 5398-5406 |
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| Format: | Online-Aufsatz |
| Sprache: | English |
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2018
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| Zugriff auf das übergeordnete Werk: | Geophysical research letters |
| Schlagworte: | Journal Article lithosphere‐asthenosphere melt ocean scattered waves seismology thermal |
| Online verfügbar |
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