Estructura del sector de Zafraimplicaciones en la subdivisión de unidades Cámbricas de la Zona de Ossa Morena (ZOM).

  1. Eguiluz, L. 1
  2. Apraiz, A. 1
  3. Martínez-Torres, L.M. 1
  4. Palacios, T. 2
  1. 1 Universidad del País Vasco/Euskal Herriko Unibertsitatea
    info
    Universidad del País Vasco/Euskal Herriko Unibertsitatea

    Lejona, España

    ROR https://ror.org/000xsnr85

    Geographic location of the organization Universidad del País Vasco/Euskal Herriko Unibertsitatea
  2. 2 Universidad de Extremadura
    info
    Universidad de Extremadura

    Badajoz, España

    ROR https://ror.org/0174shg90

    Geographic location of the organization Universidad de Extremadura
Journal:
Geogaceta

ISSN: 0213-683X

Year of publication: 1997

Issue Title: 22ª Sesión Científica, Bilbao 1997

Issue: 22

Pages: 58-62

Type: Article

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Abstract

Detailed geological mapping of the Zafra Sector (central Ossa Morena Zone, ZOM) has shown the occurrence of a minor synclinal-anticlinal coupled structure compatible with the major structure of the Monesterio Antiform. It has been observed that the Alconera and Zafra units are indeed the same unit, whereas the Los Santos Iimestone corresponds to the Sierra Gorda and Alconera Iimestones. These observations may be done extensive to the whole northern limb of the Monesterio Antiform. A revision of classical tectonic units and stratigraphic sequences, appears, therefore, needed in order to a correct analyse of Lower Paleozoic paleogeography within the Ossa Morena Zone.

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