Calibración temporal del Ordovícico Superior en el Sinclinal de Cañaveral, Monfragüe (Zona Centroibérica)

  1. Martín Garrido Susaño 1
  2. Pedro Barba Regidor 1
  1. 1 Universidad de Salamanca
    info
    Universidad de Salamanca

    Salamanca, España

    ROR https://ror.org/02f40zc51

    Geographic location of the organization Universidad de Salamanca
Journal:
Geogaceta

ISSN: 0213-683X

Year of publication: 2023

Issue: 73

Pages: 51-54

Type: Article

DOI: 10.55407/GEOGACETA95278 DIALNET GOOGLE SCHOLAR lock_openOpen access editor

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Abstract

The Cañaveral Syncline in the Monfragüe National Park contains a complete Ordovician series, where the Upper Ordovician presents one of the most complete and best exposed sections of the Central Iberian Zone (ZCI). The detailed stratigraphic study of the series has made it possible to differentiate two major formations; the Puente del Cardenal Formation and the Villarreal de San Carlos Formation, as well as to recognise the sedimentary environments, significant surfaces and sedimentary crusts. By means of sequence stratigraphy, these surfaces have been calibrated by relating them to glacioeustatic variations deduced from the isotopic curves of Begström et al. (2009).