Add to ORKGThe aim of this excursion is to show the Devonian and Carboniferous reefal development in the Cantabrian Mountains. For this purpose, several selected localities, mostly in reefal facies, will be visited. In spite of the abundance of coral and stromatoporoid faunas in the Devonian of the Cantabrian Zone, these faunas have been studied in detail only recenlly
The Devonian succession between the Guadiana and Guadalquivir Valleys in the Obejo-Valsequillo Domai...
p. 23-33Las Formaciones Candás y Portilla (Givetiense-Frasniense inferior) son dos unidades lateralm...
Conodonts have been extracted from calcareous units of the Devonian and Lower Carboniferous sequence...
The Devonian record of the Cantabrian Zone (NW SpainJ is formed of an alternation of siliciclastic a...
Devonian rocks in the Cantabrian Zone (NW Spain) are well known for their abundant content in reefal...
Centro de Informacion y Documentacion Cientifica (CINDOC). C/Joaquin Costa, 22. 28002 Madrid. SPAIN ...
Devonian reef faunas in the Cantabrian Zone are well known through several works done by the Resear...
In the Cantabrian Zone (NW Spain), as in other North Gondwanan regions, the first Devonian stage of ...
After a short introduction on the reef development during the Late Palaeozoic, the tectono-stratigra...
Within the Cantabrian zone during the Devonian and Early Carboniferous three large palaeogeographica...
The Santa Lucía Formation represents the major phase in Devonian reef development of the Cantabrian ...
The oldest reefal episode in the Cantabrian Zone (earliest Pragian) consists of small biostromal pat...
The record of Lower and Middle Devonian sedimentation in the SW border of the Iberian Massif is scar...
Two species of Lower Devonian rugose corals are described from the Cantabrian Mountains of Spain: Ca...
Three members are informally distinguished in this formation (A, B, and C from base to top). They ar...
The Devonian succession between the Guadiana and Guadalquivir Valleys in the Obejo-Valsequillo Domai...
p. 23-33Las Formaciones Candás y Portilla (Givetiense-Frasniense inferior) son dos unidades lateralm...
Conodonts have been extracted from calcareous units of the Devonian and Lower Carboniferous sequence...
The Devonian record of the Cantabrian Zone (NW SpainJ is formed of an alternation of siliciclastic a...
Devonian rocks in the Cantabrian Zone (NW Spain) are well known for their abundant content in reefal...
Centro de Informacion y Documentacion Cientifica (CINDOC). C/Joaquin Costa, 22. 28002 Madrid. SPAIN ...
Devonian reef faunas in the Cantabrian Zone are well known through several works done by the Resear...
In the Cantabrian Zone (NW Spain), as in other North Gondwanan regions, the first Devonian stage of ...
After a short introduction on the reef development during the Late Palaeozoic, the tectono-stratigra...
Within the Cantabrian zone during the Devonian and Early Carboniferous three large palaeogeographica...
The Santa Lucía Formation represents the major phase in Devonian reef development of the Cantabrian ...
The oldest reefal episode in the Cantabrian Zone (earliest Pragian) consists of small biostromal pat...
The record of Lower and Middle Devonian sedimentation in the SW border of the Iberian Massif is scar...
Two species of Lower Devonian rugose corals are described from the Cantabrian Mountains of Spain: Ca...
Three members are informally distinguished in this formation (A, B, and C from base to top). They ar...
The Devonian succession between the Guadiana and Guadalquivir Valleys in the Obejo-Valsequillo Domai...
p. 23-33Las Formaciones Candás y Portilla (Givetiense-Frasniense inferior) son dos unidades lateralm...
Conodonts have been extracted from calcareous units of the Devonian and Lower Carboniferous sequence...