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Structure géologique superficielle et évolution récente de la dorsale apulienne (Mer Ionienne)
Mascle, J.; Auroux, Ch.; Rossi, S. (1984). Structure géologique superficielle et évolution récente de la dorsale apulienne (Mer Ionienne). Rev. Inst. Fr. Pét. 39(2): 127-142
In: Revue de l'Institut Français du Pétrole. Institut Français du Pétrole, IFP: Paris. ISSN 0020-2274
Beschikbaar in  Auteurs 
Trefwoorden
    Distribution > Sediment distribution
    Earth sciences > Geology > Tectonics
    MED, Ionian Sea
    Records > Analog records > Seismic profiles
    Topographic features > Submarine features > Continental margins
    Topographic features > Submarine features > Ridges > Submarine ridges
    Topography > Topography (geology) > Bottom topography
    Ionische Zee [Marine Regions]
    Marien/Kust
Auteurs  Top 
  • Mascle, J.
  • Auroux, Ch.
  • Rossi, S.
Abstract
    The submerged Apulian Swell constitutes a wide, dissymmetric NW-SE trending topographic height extending from Apulia to Kephalinia in the northern Ionian Sea. It separates the relatively shallow southern Adriatic basin from the deeper Ionian Sea. A systematic survey (including dredging and seismic profiling) has been made by IGM Bologna across the whole area to study its sedimentary cover and shallow structure and to determine its general recent evolution. The different maps of the swell show two margins. Towards the NE (Adriatic margin) the Apulian slope is gentle, wide and sedimented. Toward the SW (Ionian margin) the slope comprises a series of steep scarps facing the deep Ionian basin and the Taranto Valley.
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