Deformación contractiva del margen noroeste ibéricoImplicaciones tectónicas del estudio paleomagnético de la Cuenca de As Pontes (NW España).

  1. Huerta, A. 1
  2. Parés, J.M. 2
  3. Cabrera, L. 3
  4. Ferrús, B. 1
  5. Sáez, A. 1
  1. 1 Universitat de Barcelona
    info

    Universitat de Barcelona

    Barcelona, España

    ROR https://ror.org/021018s57

  2. 2 lnstitut de Ciencies de la Terra Jaume Almera
  3. 3 Grup de Geodinámica i analisis de Congues Dep. de Geologia dina.mica, Geofisica i Paleontologia, Universitat de Barcelona
Erakutsi afiliazioak +
Aldizkaria:
Geogaceta

ISSN: 0213-683X

Argitalpen urtea: 1996

Zenbakien izenburua: Comunicaciones presentadas en el IV Congreso Nacional de Geología, Alcalá de Henares, 1996

Zenbakia: 20

Orrialdeak: 939-942

Mota: Artikulua

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Beste argitalpen batzuk: Geogaceta

Laburpena

The magnetochronology of the syntectonic sedimentary infilling of the Tertiary Basin of As Pontes (Northwest Spain) has allowed to determine that the activity of the NW-SE dextral strike-slip faults systems of Galicia affecting the NW margin of the Iberian Plate from the upper most Early Oligocene (Upper took placa Stampian) to the Early Miocene (Upper Aquitanian). The end of the movement of these fault systems coincides with the end of activity of the NW Iberian plate boundary acording to the sea-floor magnetic anoma/ies. Thus the end of the offshore tectonic activity was corval with its end in the NW Spanish onshore.

Datuen iturria: Dialnet