El surco calcarenítico intraplataforma de Desamendiorigen y evolución (Aptiense inferior, Aralar-Navarra)

  1. Millán Sánchez, María Isabel
  2. Agirrezabala Mundiñano, Luis M.
  3. Fernández Mendiola, Pedro Angel
  4. García Mondéjar, Joaquín
Revista:
Geotemas (Madrid)

ISSN: 1576-5172

Any de publicació: 2005

Títol de l'exemplar: XV Congreso Nacional de Sedimentología y IV Coloquio de Estratigrafía y Paleogeografía del Pérmico y Triásico de España

Número: 8

Pàgines: 73-76

Tipus: Article

Altres publicacions en: Geotemas (Madrid)

Resum

The Sagastarri limestones from the Lower Aptian of Aralar Mountains (eastern Basque-Cantabrian region, northern Spain), mainly consist of rudist, coral and orbitolinid micrites (Urgonian facies). In Desamendi area, a calcarenitic lithosome 1 km wide and 172 m thick, within the Sagastarri unit, shows lateral changes to two platform micritic limestones, through indentation, with clinoforms up to 20 m in relief. Vertical section measurements reveal a local thickness increase from West to East. Calcarenites are interpreted to fill a sysedimentary trhrough created by local differences in subsidence rates.