Estratigrafía del Mioceno Medio y Superior al NW de Crevillente (Alicante)

  1. J.E. Tent-Manclús 1
  2. Carlos Lancis 1
  3. Alfonso Yébenes 1
  4. Antonio Estévez 1
  1. 1 Universitat d'Alacant
    info

    Universitat d'Alacant

    Alicante, España

    ROR https://ror.org/05t8bcz72

Aldizkaria:
Geotemas (Madrid)

ISSN: 1576-5172

Argitalpen urtea: 2004

Zenbakien izenburua: VII Congreso Geológico de España

Zenbakia: 7

Orrialdeak: 185-190

Mota: Artikulua

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Beste argitalpen batzuk: Geotemas (Madrid)

Laburpena

The stratigraphy and nanofossil assemblages of the southern border of the Crevillente Sierra, Els Pontets section, is studied. The Miocene succession can be divided in several lithologic units: El Castellä limestones (early-middle Serravallian), Les Moreres Marls Em (middle-late Serravallian), Raya del Búho Conglomerates and Calcarenites Em (Serravallian ?- early Tortonian), Galerfa de los Suizos marls (middle-late Tortonian), and the Ventanas limestones (latest Tortonian). The lower marly interval, Les Moreres Marls Fm, can be correlated with the lower "tap marls"; the upper interval, Calería de los Suizos marls, with the upper "tap marls".

Datuen iturria: Dialnet