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| Pautot, G; Coutelle, A; Guennoc, P; Lyberis, N; Auclair, G; Berthelot, F; Dufrien, N; Parize, O. |
| New bathymetric, geologic and geophysical data obtained during the R.V. Jean Charcot Transmerou cruise in the northern Red Sea lead to a regional synthesis of the geology of this segment. Detailed surveys of the Mabahiss Deep (near 25 degree 20N) Shaban Deep (Jean Charcot near 26 degree 13N) and the Red Sea-Aqaba Suez, triple junction were made during the cruise. Ship's tracks of Transmerou are represented. |
| Tipo: Text |
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| Ano: 1990 |
URL: http://archimer.ifremer.fr/doc/00268/37953/36034.pdf |
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| Le Pichon, X; Huchon, P; Angelier, J; Lyberis, N; Boulin, J; Bureau, D; Cadet, J P; Blanchet, R; Montadert, L; Dercourt, J; Glacon, G; Got, H; Karig, D; Mascle, J; Ricou, Le; Thiebault, F. |
| Active deformation of the sea-floor of the Hellenic trench has been observed using the Cyana SP-3000 submersible. The strain pattern observed on a scale of a few kilometers is similar to the one deduced from an analysis of Seabeam morphological maps on a scale of tens of kilometers. The overall strain pattern is compatible with subduction of the Mediterranean sea-floor toward the northeast. It is characterized by underthrusting in the Western Ionian branch and left-lateral strike-slip faulting in the Eastern Strabo branch. |
| Tipo: Text |
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| Ano: 1981 |
URL: http://archimer.ifremer.fr/doc/00246/35697/34205.pdf |
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