Reinterpretación paleoambiental de la Formación Camarillas en la subcuenca de Galve (Barremiense, Cordillera Ibérica)

  1. R. Navarrete 1
  2. A.R. Soria 1
  3. C.L. Liesa 1
  4. J.P. Rodríguez-López 2
  1. 1 Universidad de Zaragoza
    info

    Universidad de Zaragoza

    Zaragoza, España

    ROR https://ror.org/012a91z28

  2. 2 University of South Wales
    info

    University of South Wales

    Pontypridd, Reino Unido

    ROR https://ror.org/02mzn7s88

Aldizkaria:
Geotemas (Madrid)

ISSN: 1576-5172

Argitalpen urtea: 2016

Zenbakien izenburua: IX CONGRESO GEOLÓGICO DE ESPAÑA

Zenbakia: 16

Orrialdeak: 233-236

Mota: Artikulua

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Beste argitalpen batzuk: Geotemas (Madrid)

Laburpena

The Camarillas Formation in the Galve sub-basin isa thick unit(> 300 m)mainly consisting ofsiliciclastic deposits (shales and sandstones) and scarcedevelopment of carbonatefacies. The study of sedimentary facies has allowed therecognitionof30 facies associations of transitional environments and,based on their lateral and vertical relationships,thecharacterization of itsstratigraphic architecture. We reinterpretthe sedimentary environment of the Camarillas Fm and distinguish three main sedimentary stages in its evolution. Stage 1 represents a tide-dominated estuary with fluvial and, then, tidal facies. Stage 2 is a tide-and wave-dominated estuary with internal, central and distal and more open marinefacies. Stage 3 isa barrier island-lagoon system in which facies associations of internal, external and open marinesubenvironmentsof the system have been recognized.

Datuen iturria: Dialnet