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

Daniel Rey García, José Bienvenido Díez Ferrer

  • 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.


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