Secuencias marino-continentales cuaternarias en el litoral del Alentejo portugués

  1. José L. Goy 1
  2. C. Zazo 2
  3. C.J. Dabrio 3
  4. D. Moura 4
  5. T. Boski 4
  6. Elvira Roquero 5
  7. A. Martínez-Graña 1
  8. Javier Lario 6
  9. Teresa Bardají 7
  1. 1 Universidad de Salamanca
    info

    Universidad de Salamanca

    Salamanca, España

    ROR https://ror.org/02f40zc51

  2. 2 Museo Nacional de Ciencias Naturales, CSIC
  3. 3 Universidad Complutense de Madrid
    info

    Universidad Complutense de Madrid

    Madrid, España

    ROR 02p0gd045

  4. 4 Universidade do Algarve
    info

    Universidade do Algarve

    Faro, Portugal

    ROR https://ror.org/014g34x36

  5. 5 Universidad Politécnica de Madrid
    info

    Universidad Politécnica de Madrid

    Madrid, España

    ROR https://ror.org/03n6nwv02

  6. 6 Universidad Nacional de Educación a Distancia
    info

    Universidad Nacional de Educación a Distancia

    Madrid, España

    ROR https://ror.org/02msb5n36

  7. 7 Universidad de Alcalá
    info

    Universidad de Alcalá

    Alcalá de Henares, España

    ROR https://ror.org/04pmn0e78

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Book:
XV Reunión Nacional de Cuaternario Bizkaia Aretoa: Bilbao, 1-5 julio 2019. Libro de resúmenes

Publisher: Universidad del País Vasco = Euskal Herriko Unibertsitatea

ISBN: 978-84-17713-16-4

Year of publication: 2019

Pages: 446-449

Congress: Reunión Nacional de Cuaternario (15. 2019. Bilbao)

Type: Conference paper

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Abstract

A detailed geomorphological map allowed to define the complex relationships between the morphostructural framework and the development of sedimentary units both marine and terrestrial along the Quaternary in the littoral area of the Alentejo (Portugal). Outcrops along Ribª do Morgadel and River Mira allowed to reconstruct a sequence of up to fourteen staircased marine terraces. In the beach of Pessegueiro Fort, a beach-dune sequence has been attributed to MIS5 in basis of OSL, 14C and U-series dating, with the beach being located at +0.5m. At Praia da Pegada, another beach deposit located at +2-4 m, has been attributed to MIS5. This chronology postdatesprevious chronological interpretations

Data source: Dialnet