Results 111 to 120 of about 2,939 (195)

New insights from U–Pb zircon dating of Early Ordovician magmatism on [PDF]

, 2008
The Central Iberian–Ossa-Morena transition zone (SW Iberian Massif) represents a segment of the northern Gondwana margin with a long geodynamic evolution, characterized by the superposition of Cadomian and Variscan events.
Bea, Fernando, Montero, Pilar, Neiva, Ana M.R., Pereira, M. Francisco, Ribeiro, Luisa, Sola, A. Rita, Williams, Ian S., Zinger, T.   +7 more
core  

The extinct shark, <i>Ptychodus</i> (Elasmobranchii, Ptychodontidae) in the Upper Cretaceous of central-western Russia-The road to easternmost peri-Tethyan seas. [PDF]

J Vertebr Paleontol, 2023
Amadori M, Solonin SV, Vodorezov AV, Shell R, Niedźwiedzki R, Kriwet J.   +5 more
europepmc   +1 more source

Late orogenic carboniferous extensions in the Variscan French Massif Central

, 1995
International audienceThe Variscan French Massif Central experienced two successive stages of extension from Middle Carboniferous to Early Permian. In the northern Massif Central, the first stage began in the late Visean, immediately after nappe stacking,
Alabouvette, Arthaud, Audrain, Barbarin, Bayer, Becq-Giraudon, Bernard-Griffiths, Berthe, Berthier, Binon, Blès, Blès, Bogdanoff, Bonijoly, Bonnion, Bouchez, Boutin, Broutin, Brun, Burg, Burg, Burg, Caen-Vachette, Carmignani, Carpena, Cassard, Cheilletz, Costa, Couturié, De Waard, Demange, Deroin, Dewey, Dewey, Didier, Dumas, Dupraz, Duthou, Duthou, Duthou, Délénin, Echtler, Echtler, Fabre, Faure, Faure, Faure, Faure, Faure, Faure, Faure, Fayol, Feist, Feix, Fernandez, Feybessse, Feys, Floc'h, Forestier, Freytet, Gagny, Gapais, Gibbs, Gras, Grolier, Grolier, Gélard, Hamet, Hollinger, Hutton, Labernardière, Lafont, Lagarde, Lameyre, Lameyre, Ledru, Ledru, Ledru, Legrand, Leistel, Lerouge, Lespinasse, Malavieille, Malavieille, Maluski, Mattauer, Matte, Mollier, Mollier, Montel, Mouctar, Ménard, Paterson, Paterson, Petitpierre, Pin, Pons, Prager, Quenardel, Rey, Robert, Rolin, Santallier, Schuilling, Thompson, Turland, Vallé, Van den Driessche, Van den Driessche, Vasseur, Vetter, Vialette, Vigneresse, Vissers, Vivier   +114 more
core   +3 more sources

Mapping a hidden terrane boundary in the mantle lithosphere with lamprophyres. [PDF]

Nat Commun, 2018
Dijkstra AH, Hatch C.
europepmc   +1 more source

The last battle of Anne of Brittany: Solving mass grave through an interdisciplinary approach (paleopathology, biological anthropology, history, multiple isotopes and radiocarbon dating). [PDF]

PLoS One, 2021
Colleter R, Bataille CP, Dabernat H, Pichot D, Hamon P, Duchesne S, Labaune-Jean F, Jean S, Le Cloirec G, Milano S, Trost M, Steinbrenner S, Marchal M, Guilbeau-Frugier C, Telmon N, Crubézy É, Jaouen K.   +16 more
europepmc   +1 more source

Early Ordovician Magmatism in the northern Central Iberian Zone (Iberian Massif): New U-Pb (SHRIMP) ages and isotopic Sr-Nd data [PDF]

, 2011
Depto. de Mineralogía y PetrologíaFac.
Castiñeiras García, Pedro, Navidad Fernández de la Cruz, Marina   +1 more
core   +1 more source

U-Pb zircon geochronology and phase equilibria modelling of HP-LT rocks in the Ossa-Morena Zone, Portugal. [PDF]

Int J Earth Sci, 2020
Akker IV, Tajčmanová L, Marques FO, Burg JP.   +3 more
europepmc   +1 more source

Seismicity of the Armorican Massif : relocations and tectonic interpretation

, 2006
Le Massif Armoricain est un segment affleurant de la Chaîne Hercynienne d'Europe Occidentale et constitue actuellement un domaine de déformation intraplaque en contexte de marge continentale passive. Cette déformation se manifeste par une activité sismique modérée caractérisée par des séismes de faible magnitude.
openaire   +1 more source

Impact of climate changes during the last 5 million years on groundwater in basement aquifers. [PDF]

Sci Rep, 2015
Aquilina L, Vergnaud-Ayraud V, Les Landes AA, Pauwels H, Davy P, Pételet-Giraud E, Labasque T, Roques C, Chatton E, Bour O, Ben Maamar S, Dufresne A, Khaska M, Le Gal La Salle C, Barbecot F.   +14 more
europepmc   +1 more source

Geomorphological evolution of the Armorican Massif since 200 Ma

, 2014
Le Massif armoricain est un domaine de socle cadomo-varisque ouest-européen de faible altitude (maximum 400m), caractérisé par des surfaces d'aplanissement, dont l'évolution géologique et géomorphologique mésozoïque et cénozoïque est débattue. L'objectif de cette étude est de reconstituer la croissance du relief de ce massif.
openaire   +1 more source