El límite meridional de la transgresión cenomaniense superior en la Cordillera Ibérica (Murcia, Albacete y Valencia)

  1. Rocio Giménez Fernández 1
  2. María del Carmen Arias Fernández 2
  3. Lorenzo Vilas Milo9ndo 3
  1. 1 Departamento Estratigrafía. IGE. Facultad Ciencias Geológicas. Mad
  2. 2 Instituto de Geologia Económica. CSIC. Madrid
  3. 3 Departamento Estratigrafía. IGE. Facultad Ciencias Geológicas. Madri
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Journal:
Geogaceta

ISSN: 0213-683X

Year of publication: 1988

Issue: 4

Pages: 23-24

Type: Article

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Abstract

During Late Cenomanian, an Atlantic transgression occurs as a result of the Iberian Plate tilting. Its southern limit is recognized in the Murcia-Albacete-Valencia area, with continental sediments, which are dividing the Iberian and Betic basins during that age.

Data source: Dialnet