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Premiers résultats de la campagne de sismique réflexion multitrace Prismed à travers la branche ionienne de la Ride Méditerranéenne
Mascle, J.; Chaumillon, E.; Hoffmann, H.J.; Rehault, J.P. (1994). Premiers résultats de la campagne de sismique réflexion multitrace Prismed à travers la branche ionienne de la Ride Méditerranéenne. C. r. Acad. sci., Sér. 2, Sci. terre planètes 318(5): 651-657
In: Comptes Rendus de l'Académie des Sciences. Série IIA. Sciences de la Terre et des Planètes = Earth and Planetary Science. Gauthiers-Villars: Paris. ISSN 1251-8050; e-ISSN 1778-4107, meer
Peer reviewed article  
Beschikbaar in  Auteurs 
Trefwoorden
    Accretion
    Earth sciences > Geology > Tectonics
    Exploration > Geophysical exploration > Seismic exploration > Profiling > Seismic reflection profiling
    MED, Mediterranean Ridge
    Phanerozoic > Geological time > Cenozoic > Tertiary > Cenozoic > Neogene > Miocene > Messinian
    Topographic features > Submarine features > Ridges > Submarine ridges
    Topographic features > Submarine features > Ridges > Submarine ridges > Mid-ocean ridges
    East Mediterranean Ridge [Marine Regions]
    Marien/Kust
Auteurs  Top 
  • Mascle, J.
  • Chaumillon, E.
  • Hoffmann, H.J.
  • Rehault, J.P.
Abstract
    A recent multichannel seismic line collected during the PRISMED cruise (March 1993) across the western branch of the Mediterranean Ridge (Central Mediterranean) allows interpretation of this feature as a tectono-sedimentary accretionary prism. Seismic processing however clearly demonstrates that most of the tectonic shortening is due to thrusting and piling up of Messinian evaporite sediments. The main decollement level could be located near the basis of Messinian evaporites.
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