Tectonic evolution of Variscan Iberia: gondwana–Laurussia collision revisited
An integrated interpretation of the late Paleozoic structural and geochronological record of
the Iberian Massif is presented and discussed under the perspective of a Gondwana …
the Iberian Massif is presented and discussed under the perspective of a Gondwana …
A review of the arcuate structures in the Iberian Variscides; constraints and genetic models
ABSTRACT In the Iberian Variscides several first order arcuate structures have been
considered. In spite of being highly studied their characterization, formation mechanisms …
considered. In spite of being highly studied their characterization, formation mechanisms …
North-Gondwana assembly, break-up and paleogeography: U–Pb isotope evidence from detrital and igneous zircons of Ediacaran and Cambrian rocks of SW Iberia
The Estremoz Anticline in the Ossa-Morena Zone (SW Iberia) includes upper Ediacaran
detrital rocks unconformably overlain by lower Cambrian detrital and carbonate rocks. The …
detrital rocks unconformably overlain by lower Cambrian detrital and carbonate rocks. The …
Variscan ophiolite belts in the Ossa-Morena Zone (Southwest Iberia): Geological characterization and geodynamic significance
The boundary between the Iberian and South-Portuguese terranes in SW Iberia is traced by
a suture recording the closure of Rheic and related oceans through NNE-directed …
a suture recording the closure of Rheic and related oceans through NNE-directed …
Early Ordovician–Devonian passive margin stage in the Gondwanan units of the Iberian Massif
JC Gutiérrez-Marco, JM Piçarra, CA Meireles… - The Geology of Iberia: A …, 2019 - Springer
Progressive opening of the Rheic Ocean led to the drifting away of one or several ribbon
terranes, generally ascribed to Avalonia, and inaugurated a passive margin stage on the …
terranes, generally ascribed to Avalonia, and inaugurated a passive margin stage on the …
Synorogenic basins
JT Oliveira, E González-Clavijo, J Alonso… - The Geology of Iberia: A …, 2019 - Springer
Synorogenic basins formed in all lithospheric units involved in the Variscan orogeny, ie the
Gondwanan and Laurussian continental margins and also in the oceanic realm. However …
Gondwanan and Laurussian continental margins and also in the oceanic realm. However …
Variscan metamorphism
ML Ribeiro, J Reche, A López-Carmona… - The Geology of Iberia: A …, 2019 - Springer
Various segments of Variscan crust are currently exposed in Iberia in response to
successive tectonic events during the Variscan orogeny itself and subsequent extensional …
successive tectonic events during the Variscan orogeny itself and subsequent extensional …
SW Iberia Variscan suture Zone: oceanic affinity units
C Quesada, JA Braid, P Fernandes, P Ferreira… - The Geology of Iberia: A …, 2019 - Springer
The geology of SW Iberia records a sequence of geologic events from the Cambrian-Early
Ordovician rifting and subsequent passive margin development along the southern flank of …
Ordovician rifting and subsequent passive margin development along the southern flank of …
Stratigraphy of the Northern Pulo do Lobo Domain, SW Iberia variscides: A palynological contribution
We present palynological results from the northern sector of the Pulo do Lobo Domain,
combining sections studied in Portugal and Spain. A total of 139 samples were studied, of …
combining sections studied in Portugal and Spain. A total of 139 samples were studied, of …
Evolução geodinâmica da Zona de Ossa-Morena no contexto do SW Ibérico durante o Ciclo Varisco
A evolução geodinâmica da Zona de Ossa-Morena é essencial na compreensão do Ciclo
Varisco no Terreno Autóctone Ibérico. Vários estudos de índole estratigráfica, estrutural …
Varisco no Terreno Autóctone Ibérico. Vários estudos de índole estratigráfica, estrutural …