Situé .sur la côte Nord-Est du Massif Armoricain et partiellementimmergé dans sa partie septentrionale (fig. 1), le Massif de St•Malo constitue un complexe métamorphique â la limite des domainesmancellien et domnonéen (COGNE, 1974) •Par son orientation cartographique N 60° il possède une. certaineoriginalité dans le ccl1texte géologique armoricain, que
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Dome-headed, small-brained island mammal from the Late Cretaceous of Romania. [PDF]
Csiki-Sava Z +4 more
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Nine taxa of rugose corals collected by LEMAÎTRE (1934) and coming from the Chalonnes Formation of the Southeastern Armorican Massif in France have been revised.
Coen-Aubert, M.
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Formation of low-pressure reaction textures during near-isothermal exhumation of hot orogenic crust (Bohemian Massif, Austria). [PDF]
Sorger D +5 more
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Island life in the Cretaceous - faunal composition, biogeography, evolution, and extinction of land-living vertebrates on the Late Cretaceous European archipelago. [PDF]
Csiki-Sava Z +4 more
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Jury: Guilhem Barruol Examinateur Jean-Pierre Brun Invité Michel Granet Directeur de thèse Eduard Kissling Rapporteur externe Patrick Ledru Rapporteur externe Gérard Wittlinger Rapporteur interneThe Hercynian Range is a major object of the european ...
Judenherc, Sébastien
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Digestive and appendicular soft-parts, with behavioural implications, in a large Ordovician trilobite from the Fezouata Lagerstätte, Morocco. [PDF]
Gutiérrez-Marco JC +3 more
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Biogeochemical prospecting of metallic critical raw materials: soil to plant transfer in SW Ciudad Real Province, Spain. [PDF]
Barquero JI +6 more
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Divergence in the evolution of Paleolithic symbolic and technological systems: The shining bull and engraved tablets of Rocher de l'Impératrice. [PDF]
Naudinot N +7 more
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STORM DEPOSITS: THE MODEL OF THE MIDDLE ORDOVICIAN OF THE WESTERN ARMORICAN MASSIF
Among rescdimentation proccsses, tcmrests have bren recognized since several yeara as an import11nt phenomenon in the constitution of shelf sedimentary series Two types of sedimcntary figures are nowadays considered as caracteristic of this kind of deposit : hummocky cross-stratification or HCS (Harm, 1975) nnd storm graded-layers .
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