Edification processes of an interlobe unit: application to the Rhone deep-sea fan (France)
The Rhone deep-sea fan is formed by the superposition of lenticular units, sedimentary ridges or fan lobes This study deals with a depositional unit adjacent to the main fan called "Unite Interlobe". Bathymetric data (Seabeam), high resolution seismic profiling (Airgun, Sparker and 3.5 kHz...
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| Veröffentlicht in: | Comptes rendus de l'Académie des sciences. Série 2, Mécanique, physique, chimie, sciences de l'univers, sciences de la terre Mécanique, physique, chimie, sciences de l'univers, sciences de la terre, 1993-01, Vol.317 (12) |
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| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | fre |
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| Online-Zugang: | Volltext |
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| Zusammenfassung: | The Rhone deep-sea fan is formed by the superposition of lenticular units, sedimentary ridges or fan lobes This study deals with a depositional unit adjacent to the main fan called "Unite Interlobe". Bathymetric data (Seabeam), high resolution seismic profiling (Airgun, Sparker and 3.5 kHz) supplemented by piston-core sampling show that the "Unite Interlobe" is a composite construction, of relatively recent age, resulting from alternating channelization and slumping processes. |
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| ISSN: | 0764-4450 |