RT Journal Article
T1 Rasgos estratigráficos de la sucesión del Ordovícico Superior en Portilla de Luna (Zona Cantábrica, noroeste de España)
T1 The Upper Ordovician sequence of Portilla de Luna (Canlabrian Tone, NW Spain)
A1 Gutiérrez Marco, Juan Carlos
A1 Aramburu, C.
A1 Arbizu, M.
A1 Méndez Bedia, I.
A1 Rábano, Isabel
A1 Villas, E.
AB Upper Ordovician rocks have been characterized for the first time in the Cantabrian Zone of the Hesperian Massif. The sequence consists of a lower siliciclastic unit of Caradoc-(‘basal Ashgill age developed as an alternation of shales, siltstones and sandstones, overlain by an upper unit of fossiliferous limestones with marly intercalations, of pre-Hirnantian (mainly Cautleyan-Rawtheyan) age. Ashgill fossils are fairly abundant in the limestone unit, and there have been identified brachiopods of the «Nicolella fauna», echinoderms of the «Heliocrinites fauna» and trilobites of the Qvalocephalus biofacies
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/11425
UL http://hdl.handle.net/10272/11425
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026