Add to ORKGThe Devonian succession between the Guadiana and Guadalquivir Valleys in the Obejo-Valsequillo Domain comprises more than 600 m of shale and sandstone with some interbedded limestone and marl. The most complete sequences are located in the Guadámez-2, Arroyo del Lobo, Zújar, Peñón Cortado and Arroyo del Pozo del Rincón sections. Pragian reefal facies occur at most of these localities but Emsian reefs are well developed only in the Guadámez-2 section
The Brilon-reef complex is one of the biggest Devonian carbonate buildups (similar to 80 km(2)) of t...
Relative sea level fluctuations during the Frasnian generated two shallow-marine, mixed siliciclasti...
The oldest reefal episode in the Cantabrian Zone (earliest Pragian) consists of small biostromal pat...
The Devonian record of the Cantabrian Zone (NW SpainJ is formed of an alternation of siliciclastic a...
Lack of adequately palaeontological studies, complex tectonics and discontinuous outcrops difficult ...
The aim of this excursion is to show the Devonian and Carboniferous reefal development in the Canta...
The record of Lower and Middle Devonian sedimentation in the SW border of the Iberian Massif is scar...
In the Cantabrian Zone (NW Spain), as in other North Gondwanan regions, the first Devonian stage of ...
p. 23-33Las Formaciones Candás y Portilla (Givetiense-Frasniense inferior) son dos unidades lateralm...
The Santa Lucía Formation represents the major phase in Devonian reef development of the Cantabrian ...
Devonian rocks in the Cantabrian Zone (NW Spain) are well known for their abundant content in reefal...
Devonian reef faunas in the Cantabrian Zone are well known through several works done by the Resear...
The Asturo-Leonese Basin is one of the three large palaeogeographical units of the Cantabrian Zone. ...
Centro de Informacion y Documentacion Cientifica (CINDOC). C/Joaquin Costa, 22. 28002 Madrid. SPAIN ...
The Brilon-reef complex is one of the biggest Devonian carbonate buildups (~80 km²) of the Rheinisch...
The Brilon-reef complex is one of the biggest Devonian carbonate buildups (similar to 80 km(2)) of t...
Relative sea level fluctuations during the Frasnian generated two shallow-marine, mixed siliciclasti...
The oldest reefal episode in the Cantabrian Zone (earliest Pragian) consists of small biostromal pat...
The Devonian record of the Cantabrian Zone (NW SpainJ is formed of an alternation of siliciclastic a...
Lack of adequately palaeontological studies, complex tectonics and discontinuous outcrops difficult ...
The aim of this excursion is to show the Devonian and Carboniferous reefal development in the Canta...
The record of Lower and Middle Devonian sedimentation in the SW border of the Iberian Massif is scar...
In the Cantabrian Zone (NW Spain), as in other North Gondwanan regions, the first Devonian stage of ...
p. 23-33Las Formaciones Candás y Portilla (Givetiense-Frasniense inferior) son dos unidades lateralm...
The Santa Lucía Formation represents the major phase in Devonian reef development of the Cantabrian ...
Devonian rocks in the Cantabrian Zone (NW Spain) are well known for their abundant content in reefal...
Devonian reef faunas in the Cantabrian Zone are well known through several works done by the Resear...
The Asturo-Leonese Basin is one of the three large palaeogeographical units of the Cantabrian Zone. ...
Centro de Informacion y Documentacion Cientifica (CINDOC). C/Joaquin Costa, 22. 28002 Madrid. SPAIN ...
The Brilon-reef complex is one of the biggest Devonian carbonate buildups (~80 km²) of the Rheinisch...
The Brilon-reef complex is one of the biggest Devonian carbonate buildups (similar to 80 km(2)) of t...
Relative sea level fluctuations during the Frasnian generated two shallow-marine, mixed siliciclasti...
The oldest reefal episode in the Cantabrian Zone (earliest Pragian) consists of small biostromal pat...