Dolomitización en materiales del tránsito Cretácico-Terciario en la Sección de Quecedo (Norte de Burgos, España).

  1. M.A. Rioja 1
  2. F. García-Garmilla 1
  3. M. Erkiaga 1
  4. J. Elorza 1
  1. 1 Departamento de Mineralogía y Petrología, Facultad de Ciencias, Universidad del País Vasco
Aldizkaria:
Geogaceta

ISSN: 0213-683X

Argitalpen urtea: 1996

Zenbakia: 20

Orrialdeak: 647-650

Mota: Artikulua

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Beste argitalpen batzuk: Geogaceta

Garapen Iraunkorreko Helburuak

Laburpena

Oiagenetic processes of dolomitization and calcitization have been recorded from the upper Maastrichtian - lower Danian shaflow-marine carbonate rocks at Quecedo. Oolomitization is associated to a first arder sequence boundary, evo/ved from upper to lower and affected very shaflow marine sediments. A diagenetic sequence from evaporative, to marine and meteoric mixing ambients, to a later freshwater generalized input can be inferred from both the study of microtextures and cathodoluminescence observations.

Datuen iturria: Dialnet