Precisiones bioestratigráficas y sedimentológicas sobre el Plioceno del norte de la Sierra de Santa Pola (Alicante)

  1. Carlos Lancis 1
  2. Alfonso Yébenes 1
  3. J.A. Flores 2
  4. J.E. Tent-Manclús 1
  1. 1 Universitat d'Alacant
    info

    Universitat d'Alacant

    Alicante, España

    ROR https://ror.org/05t8bcz72

  2. 2 Universidad de Salamanca
    info

    Universidad de Salamanca

    Salamanca, España

    ROR https://ror.org/02f40zc51

Aldizkaria:
Geotemas (Madrid)

ISSN: 1576-5172

Argitalpen urtea: 2004

Zenbakien izenburua: VII Congreso Geológico de España

Zenbakia: 7

Orrialdeak: 143-147

Mota: Artikulua

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Beste argitalpen batzuk: Geotemas (Madrid)

Laburpena

A Pliocene succession cropping out to the north of the Santa Pola cape (Bajo Segura Basin, Alicante, Spain) is studied. The pliocene materials disconformably overlie the Messinian Terminal Complex. The first pliocene unit, composed of fosiliferous silty marls, was deposited in an open shallow platform. Its nannoplankton associations points to a middle-late Zanclien age. The second unit consist of calcareous sandstones with frequent fossils and tractive structures, forming shallowing-upward sequences related to the progradation of beach systems. The last pliocene unit, quite thin, consists of fresh water lagoon marly deposits.

Datuen iturria: Dialnet