The Ordovician, Silurian and Devonian sedimentary rocks of the Ossa-Morena Zone (SW Iberian Peninsula, Spain)
JC Gutiérrez-Marco, M Robardet - 2004 - digital.csic.es
[EN] The present paper reviews the Ordovician, Silurian and Devonian sedimentary rocks of
the Ossa-Morena Zone of the SW Hesperian (Iberian) Massif in Spain and Portugal. It gives …
the Ossa-Morena Zone of the SW Hesperian (Iberian) Massif in Spain and Portugal. It gives …
The Ordovician chitinozoan biozones of the Northern Gondwana domain
F Paris - Review of Palaeobotany and Palynology, 1990 - Elsevier
A formal biozonation is proposed for the Ordovician chitinozoans of the Northern Gondwana
Domain. This palaeogeographic province, located at rather high latitudes during the …
Domain. This palaeogeographic province, located at rather high latitudes during the …
The geology of Spain
W Gibbons, T Moreno - 2002 - books.google.com
The Society makes every effort to ensure that the scientific and production quality of its
books matches that of its journals. Since 1997, all book proposals have been refereed by …
books matches that of its journals. Since 1997, all book proposals have been refereed by …
Early Palaeozoic palaeobiogeography of the Variscan regions
F Paris, M Robardet - Tectonophysics, 1990 - Elsevier
The palaeobiogeographic method appears to be an attractive alternative for reconstruction
of the palaeogeography of the Variscan regions during the Palaeozoic. The evolution of …
of the palaeogeography of the Variscan regions during the Palaeozoic. The evolution of …
Cretaceous
J Martín-Chivelet, X Berástegui, I Rosales, L Vilas… - 2002 - pubs.geoscienceworld.org
Cretaceous rocks crop out extensively in the three main Alpine orogenic belts of Spain: the
Betic Cordillera, the Pyrenees and the Iberian Ranges. These rocks, deformed during …
Betic Cordillera, the Pyrenees and the Iberian Ranges. These rocks, deformed during …
Stratigraphy
A Pérez Estaún, I Mendez Bedia… - Pre-Mesozoic Geology …, 1990 - Springer
Abstract The Cantabrian Zone can be divided into two areas from the stratigraphic point of
view: the Asturian-Leonese domain and the Palentine domain. The Asturian-Leonese …
view: the Asturian-Leonese domain and the Palentine domain. The Asturian-Leonese …
Ordovician ironstone of the Iberian margin: Coastal upwelling, ocean anoxia and Palaeozoic biodiversity
Abstract Middle to Upper Ordovician ironstone and associated sedimentary rocks of the
West Asturian‐Leonese and Cantabrian tectonostratigraphic zones, Spain, provide new …
West Asturian‐Leonese and Cantabrian tectonostratigraphic zones, Spain, provide new …
[PDF][PDF] La sedimentación cambro-ordovícica en la Zona Cantábrica (NO de España)
CI Aramburu-Zabala Higuera… - … de Geología, 19, 1993 - digibuo.uniovi.es
El Cambro-Ordovícico de la Zona Cantábrica comprende entre 2000 y 4.000 m de
sedimentos mayoritariamente siliciclásticos, con intercalaciones de carbonatos y rocas …
sedimentos mayoritariamente siliciclásticos, con intercalaciones de carbonatos y rocas …
Structure
JR Martínez Catalán, A Pérez Estaún, F Bastida… - Pre-Mesozoic Geology …, 1990 - Springer
The structural configuration of the West Asturian-Leonese Zone (W ALZ) may be appreciated
from the cross-sections of Fig. 1, the location of the main structures are depicted in Fig. 1 of …
from the cross-sections of Fig. 1, the location of the main structures are depicted in Fig. 1 of …
Lower Llanvirn (Ordovician) graptolites and acritarchs from the «assise de Huy», Bande de Sambre-et-Meuse, Belgium
T Servais, J Maletz - Annales de la Société géologique de …, 1992 - popups.uliege.be
Résumé La formation de Huy («assise de Huy») est l'unité la plus ancienne qui affleure
dans la Bande de Sambre-et-Meuse. Des graptolites et des acritarches indiquent un âge …
dans la Bande de Sambre-et-Meuse. Des graptolites et des acritarches indiquent un âge …