Ophiolites of different Paleozoic ages occur in North-West (NW) Iberia in a rootless suture representing the remnants of the Rheic Ocean. Associated allochthonous terranes in the …
Three major orogenic belts that are host to coupled oroclines (terrane wrecks) are likewise characterized by or directly associated with paleomagnetic inclination anomalies:(1) the …
JR Martínez Catalán, FJ Rubio Pascual… - Geological Society …, 2014 - lyellcollection.org
The Variscan metamorphic evolution of the autochthonous domain of NW and Central Iberia is characterized by a Barrovian gradient followed by a high-temperature–low-pressure …
Abstract The NW Iberian Allochthon and the Teplá-Barrandian and Moldanubian zones represent the internal parts of the Variscan belt in their respective domains. A correlation …
The Góry Sowie Massif (GSM) in Poland represents a Devonian high-pressure–ultrahigh- pressure (HP–UHP) terrane dominated by paragneiss, with subordinate orthogneiss …
Allochthonous ophiolitic units in the northwestern Iberian Massif are remnants of peri- Gondwanan Paleozoic oceans sandwiched among other exotic terranes of continental and …
Abstract In the Galicia Region of the NW Iberian Massif several allochthonous complexes (Cabo Ortegal, Órdenes and Malpica-Tui) contain a rootless Variscan suture that can be …
New U–Pb zircon data of a mylonitic greenschist from the Moeche Ophiolite, one of the mafic units involved in the Variscan suture in the Cabo Ortegal Complex (NW of the Iberian …
The basal allochthonous units of NW and SW Iberia are members of an intra-Gondwana suture zone that spreads across the Iberian Massif and was formed during the collision of …