Una discontinuidad estratigráfica de 6 m.a. En las calizas albienses de Aitziber (Navarra)

  1. Quintanar-Soto, A.B.
  2. Fernández-Mendiona, P.A.
  3. Caron, M.
Journal:
Geogaceta

ISSN: 0213-683X

Year of publication: 1998

Issue: 25

Pages: 171-174

Type: Article

More publications in: Geogaceta

Abstract

The Aitziber calcarenites is a sedimentary unit of Upper Albian (appenninica with buxtorfi zone) age. The top of this unit records an unconformity of at least 6 m.a.. The hiatus extends from the uppermost Albian to lower Turonian