El límite Anisiense-Ladiniense (Triásico) en el Buntsandstein de la Rama Castellana de la Cordillera Ibéricareinterpretación de los datos magnetoestratigráficos y bioestratigráficos

  1. D. Rey
  2. J.B. Díez
Aldizkaria:
Geotemas (Madrid)

ISSN: 1576-5172

Argitalpen urtea: 2000

Zenbakien izenburua: V Congreso Geológico de España (Alicante, 10-14 julio 2000)

Zenbakia: 1

Orrialdeak: 125-129

Mota: Artikulua

Beste argitalpen batzuk: Geotemas (Madrid)

Laburpena

In recent times, Muttoni et at. (1998) have proposed a refined Middle Triassic magnetostratigraphy based on biostratigraphically well constrained carbonade sequences from the Thetys realm. This together with the exhaustive revision of previous and new biostratigraphical Triassic data from the Western Peritethys Domain carried out by Diez (2000), have allowed a significant improvement in the dating of the studied upper Buntsandstein continental red bed sequences by correlation with the reference marine data.