Results 101 to 110 of about 1,408 (212)
The Eastern Galicia Magnetic Anomaly (EGMA) is one of the most distinctive and best studied magnetic anomalies in Iberia. It is located in NW Spain and overlaps the Variscan gneissic domes of Lugo and Sanabria.
Ayarza Arribas, Puy +5 more
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The Role of the Hercynian Mountains of Central Europe in Shaping Plant Migration Patterns in the Pleistocene-A Review. [PDF]
Plants (Basel), 2023 Urbaniak J, Kwiatkowski P.
europepmc +1 more source
Within the Variscan Belt of Morocco, the Central Massif preserves Early Carboniferous rift basins. The Lower Carboniferous Khenifra and Qasbat-Tadla basins are aborted rifts, developed just before the Variscan orogenesis in Morocco that occurred during ...
Ouchaou, Rachid +9 more
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About a peri-Gondwanan-North African enlarged acceptance of the Caledonian Orogeny
, 2011 The notion of “Caledonian Orogeny” is restricted by most authors to the Ordovician-Devonian thermotectonic events associated with the Laurentia-Baltica- Avalonia suturing.
Ioan Balintoni +5 more
core +1 more source
Paleozoic evolution of pre-Variscan terranes: From Gondwana to the Variscan collision
, 2005 The well-known Variscan basement areas of Europe contain relic terranes with a pre- Variscan evolution testifying to their peri-Gondwanan origin (e.g., relics of Neoproterozoic volcanic arcs, and subsequent stages of accretionary wedges, backarc ...
Stampfli, Gérard M. +2 more
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Outline of the Variscan basement of Sardinia [PDF]
, 2009 In Sardinia a quasi-complete section of the southern branch of the Variscan orogenic belt crops out, characterized by non-metamorphosed to high-grade rocks, whose age ranges from Early Cambrian to Early Carboniferous, and that are involved in a complex ...
Oggiano, Giacomo, FUNEDDA, ANTONIO LUCA
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Physical and Thermal Properties Analysis of Hematite for Thermal Heat Storage. [PDF]
Materials (Basel), 2022 Santos A, Almeida F, Rocha F.
europepmc +1 more source
GeosciencesThe Penacova-Régua-Verin (PRV) and the Manteigas-Vilariça-Bragança (MVB) are two of the longest faults of the Iberian Peninsula. These faults striking NNE–SSW, over lengths of >200 km, were developed during late-Variscan Orogeny and reactivated in ...
Sandra González-Muñoz +1 more
doaj +1 more source
Geochronology and petrogenesis of late-Variscan plutonism (NW Portugal) : synthesis and inferences on crustal recycling and growth [PDF]
, 2009 In NW Portugal large volumes of granitoids were emplaced during the post-collisional stage of the Variscan orogeny. This was the main period of successive granite generation, which exhibit different chemical and isotopic signatures.
Simões, P. P. +5 more
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, 2022 Evidence of Ordovician tectonics is well preserved in the Variscan terrains now scattered in the circum-Mediterranean areas. It was in SW Sardinia (the External Zone of the Variscan basement) that was firstly detected the so-called Sardic Phase, a ...
Casini Leonardo +8 more
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