RT info:eu-repo/semantics/conferenceObject
T1 Examples of architecture of reefal facies and related deposits in the Devonian of the Cantabrian Zone (NW Spain)
A1 Fernández, Luis Pedro
A1 Arbizu, Miguel
A1 Fernández Martínez, Esperanza
A1 García Alcalde, Jenaro Luis
A1 Méndez Bedia, Isabel
A1 Soto, Francisco
A1 Truyols Massoni, Montse
A1 Vera de la Puente, Carmen
A2 Paleontologia
K1 Paleontología
K1 Sedimentos (Geología)
K1 Devónico
K1 Cordillera Cantábrica (España)
K1 Estratigrafía
K1 Corales
K1 España
K1 Arrecifes
AB The Devonian record of the Cantabrian Zone (NW SpainJ is formed of an alternation of siliciclastic and carbonate units, chicfly of shallow water origin, that were deposited on the North Gondwanan pasive margin prior to the onset of the Variscan orogeny (Carboniferous).The carbonate units range from a few tens to some two hundred metres in thickness and record deposition in carbonate platforms of mainly ramp type. They are relatively rich in reefal faunas in such a way that seven reefal episodes ol uneven importance. spanning from earliest Pragian to Famennian, have been distinguished. These reefal episodes consist of coral and stromatoporoid bioherms and biostromes with a local appearance of niud mounds.
YR 2019
FD 2019-03-12
LK http://hdl.handle.net/10612/9746
UL http://hdl.handle.net/10612/9746
NO X Internacional Congress on Fossil Cnidaria and Porifera, 12-16 de agosto, 2007, San Petersburgo (Rusia)
DS BULERIA. Repositorio Institucional de la Universidad de León
RD 25-abr-2024