Céline Ducassou
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View article: U–Pb age constraints on the Carboniferous–Permian transition in continental basins of eastern equatorial Pangaea (France): implications for the depositional history and correlations across the late Variscan Belt
U–Pb age constraints on the Carboniferous–Permian transition in continental basins of eastern equatorial Pangaea (France): implications for the depositional history and correlations across the late Variscan Belt Open
Intramontane late Carboniferous–Permian basins of western Europe developed during the latest orogenic stages of the Variscan Mountain Belt in eastern Pangaea, at equatorial palaeolatitudes. Their stratigraphic framework is mainly based on …
View article: The Late Paleozoic Ice Age in western equatorial Pangea: Context for complex interactions among aeolian, alluvial, and shoreface sedimentary environments during the Late Pennsylvanian – early Permian
The Late Paleozoic Ice Age in western equatorial Pangea: Context for complex interactions among aeolian, alluvial, and shoreface sedimentary environments during the Late Pennsylvanian – early Permian Open
View article: U–Pb age constraints on the Carboniferous–Permian transition in continental basins of eastern equatorial Pangaea (France): implications for the depositional history and correlations across the late Variscan Belt
U–Pb age constraints on the Carboniferous–Permian transition in continental basins of eastern equatorial Pangaea (France): implications for the depositional history and correlations across the late Variscan Belt Open
Supplementary Material Table 1. ICP–MS and ICP–OES geochemistry results for the LV, LYF-416.5 and LYF-567.7 samples.
View article: U–Pb age constraints on the Carboniferous–Permian transition in continental basins of eastern equatorial Pangaea (France): implications for the depositional history and correlations across the late Variscan Belt
U–Pb age constraints on the Carboniferous–Permian transition in continental basins of eastern equatorial Pangaea (France): implications for the depositional history and correlations across the late Variscan Belt Open
Supplementary Material Table 3. LA–ICP–MS results for the LV sample (Aumance Basin).
View article: U–Pb age constraints on the Carboniferous–Permian transition in continental basins of eastern equatorial Pangaea (France): implications for the depositional history and correlations across the late Variscan Belt
U–Pb age constraints on the Carboniferous–Permian transition in continental basins of eastern equatorial Pangaea (France): implications for the depositional history and correlations across the late Variscan Belt Open
Supplementary Material Table 4. CA–ID–TIMS results for the LV, LYF-567.7 and LYF-416.5 samples.
View article: Reconsidering Carboniferous–Permian continental paleoenvironments in eastern equatorial Pangea: facies and sequence stratigraphy investigations in the Autun Basin (France)
Reconsidering Carboniferous–Permian continental paleoenvironments in eastern equatorial Pangea: facies and sequence stratigraphy investigations in the Autun Basin (France) Open
View article: A rare late Mississippian flora from Northwestern Europe (Maine-et-Loire Coalfield, Pays de la Loire, France)
A rare late Mississippian flora from Northwestern Europe (Maine-et-Loire Coalfield, Pays de la Loire, France) Open
View article: Structure of the Offshore Obducted Oman Margin: Emplacement of Semail Ophiolite and Role of Tectonic Inheritance
Structure of the Offshore Obducted Oman Margin: Emplacement of Semail Ophiolite and Role of Tectonic Inheritance Open
The northern Oman margin is a key area for understanding the emplacement of the Semail Ophiolite and obduction processes in general. This study uses a grid of 2D‐multichannel seismic lines tied to well data to characterize the offshore dom…
View article: Palaeoenvironmental reconstitutions at the Carboniferous–Permian transition south of the Paris Basin, France: implications on the stratigraphic evolution and basin geometry
Palaeoenvironmental reconstitutions at the Carboniferous–Permian transition south of the Paris Basin, France: implications on the stratigraphic evolution and basin geometry Open
View article: Le bassin intracontinental fini-carbonifère - permien de Lucenay-lès-Aix (nord-est du Massif Central) : réévaluation sédimentologique et implicationspaléoenvironnementales
Le bassin intracontinental fini-carbonifère - permien de Lucenay-lès-Aix (nord-est du Massif Central) : réévaluation sédimentologique et implicationspaléoenvironnementales Open
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View article: Data for: Sedimentology and U-Pb dating of Carboniferous to Permian continental series of the northern Massif Central (France): palaeogeographic evolution and geodynamic implications
Data for: Sedimentology and U-Pb dating of Carboniferous to Permian continental series of the northern Massif Central (France): palaeogeographic evolution and geodynamic implications Open
Table 1: Geochemical analyses Table 2: Analytical uncertainties and limits of detection for analyses provided in Table 1 Table 3: Operating and instrumental conditions for U-Pb analyses on zircon Table 4: Operating and instrumental conditi…
View article: Sedimentology and U-Pb dating of Carboniferous to Permian continental series of the northern Massif Central (France): Local palaeogeographic evolution and larger scale correlations
Sedimentology and U-Pb dating of Carboniferous to Permian continental series of the northern Massif Central (France): Local palaeogeographic evolution and larger scale correlations Open
View article: Using volcaniclastic rocks to constrain sedimentation ages: To what extent are volcanism and sedimentation synchronous?
Using volcaniclastic rocks to constrain sedimentation ages: To what extent are volcanism and sedimentation synchronous? Open
View article: Relief variation and erosion of the Variscan belt: detrital geochronology of the Palaeozoic sediments from the Mauges Unit (Armorican Massif, France)
Relief variation and erosion of the Variscan belt: detrital geochronology of the Palaeozoic sediments from the Mauges Unit (Armorican Massif, France) Open
The sediments of the Mauges Unit located in the internal zone provide an opportunity of studying the evolution of relief during Palaeozoic time. U–Pb dating on zircon and 39Ar/40Ar on white mica are used to constrain …
View article: Thermo-mechanical modeling of the obduction process based on the Oman Ophiolite case
Thermo-mechanical modeling of the obduction process based on the Oman Ophiolite case Open