Abstract
Three main structural and sedimentary provinces characterize the Nile Cone. A western domain shows a network of tightly meandering distributary channels. A central province displays numerous huge growth faults, as well as distributary channels and characteristic sedimentary structures. In both areas, widespread layers of debris-flows are present. Finally an eastern province is the locus of intense active faulting. Important salt diapirism ascends along many of the faults.
| Translated title of the contribution | The Nile Cone: Main results of the Prismed II cruise of the R.V. L'Atalante |
|---|---|
| Original language | French |
| Pages (from-to) | 727-733 |
| Number of pages | 7 |
| Journal | Comptes Rendus - Academie des Sciences, Serie II: Sciences de la Terre, et des Planetes |
| Volume | 329 |
| Issue number | 10 |
| DOIs | |
| State | Published - 30 Nov 1999 |
Keywords
- Deep-sea fans
- Eastern Mediterrannean
- Nile
- Salt diapirs
- Seismic profiling
- Swath bathymetry and imagery
ASJC Scopus subject areas
- Ecology, Evolution, Behavior and Systematics
- Ocean Engineering