Seismic Evidence for a Hot Mantle Transition Zone Beneath the Indian Ocean Geoid Low
Abstract The Indian Ocean Geoid Low (IOGL) is the most prominent geoid anomaly (−106 m) on the globe, whose origin remains elusive. In the present study, we investigate the mantle transition zone (MTZ) structure beneath the region using P receiver functions (PRFs), to examine its role in the genesis...
| Hauptverfasser: | , , |
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| Format: | Artikel |
| Sprache: | English |
| Veröffentlicht: |
Wiley
2020-07-01
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| Schriftenreihe: | Geochemistry, Geophysics, Geosystems |
| Online Zugang: | https://doi.org/10.1029/2020GC009079 |