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Marges continentales transformantes
Mascle, J., Jean; Basile, Ch., Christophe (1998). Marges continentales transformantes. Earth Planet. Sci. Lett. 326(12): 827-838
In: Earth and Planetary Science Letters. Elsevier: Amsterdam. ISSN 0012-821X; e-ISSN 1385-013X, meer
Peer reviewed article  

Beschikbaar in  Auteurs 

Trefwoorden
    Cote d'Ivoire
    Earth sciences > Geology
    Earth sciences > Geology > Tectonics
    Earth sciences > Geophysics
    Earth structure > Earth crust > Oceanic crust
    Geological structures > Faults > Transform faults
    Ghana
    ISE, Mexico, California Gulf
    Morphology
    Morphology
    Morphology
    Rifting
    Topographic features > Landforms > Ridges
    Topographic features > Submarine features > Continental margins
    Topography
    Ghana [Marine Regions]; Gulf of California [Marine Regions]; Ivorian Exclusive Economic Zone [Marine Regions]
    Marien/Kust

Auteurs  Top 
  • Mascle, J.
  • Basile, Ch.

Abstract
    We present and discuss three main stages that successively control the sedimentary, tectonic and crustal evolution along continental margin segments wbich result chielly from transform rifting between two parting continents. During an intracontinental stage, the future margin area is submitted to specific thermal and wrench tectonic activities and to a dominantly clastic sedimentation. In a second stage, an active transform contact between continental crust and a newly created oceanic crust, induces a sharp transition between ocean and continent crusts, as welt as the creation of a very steep and linear slope. Finally, the margin is submitted to a more standard cooling subsidence and accompanying sedimentation.

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