Correlación de alta resolución del Campaniense-Maastrichtiense, Pirineos sud-centrales

  1. E. Vicens
  2. L. Ardèvol
  3. N. López-Martínez
  4. M.E. Arribas
Aldizkaria:
Geotemas (Madrid)

ISSN: 1576-5172

Argitalpen urtea: 2001

Zenbakien izenburua: XIV Congreso Nacional de Sedimentología, IV Congreso del Cretácico de España

Zenbakia: 3

Orrialdeak: 261-264

Mota: Artikulua

Beste argitalpen batzuk: Geotemas (Madrid)

Laburpena

A regressive succession of deltaic, shoreface, and continental strata characterized the deposition during the Campanian-Maastrichtian time in the foreland basin of the south-central Pyrenees. This work introduces a high-resolution stratigraphic framework among these strata along the different structural sectors of the eastern part o f the basin. The framework is based on the recognition and correlation of eight calcarenitic rudist-bearing horizons intercalated within a thick siliciclastic section. These horizons, named after their most characteristic species, have been correlated with planctonic foraminifera biozones following a shelf-to-basin stratigraphic cross-section. We conclude that these rudist horizons are valid as biostratigraphic markers.