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期刊论文 [6]
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A global palaeoclimatic reconstruction for the Valanginian based on clay mineralogical and geochemical data [期刊论文]
Earth-Science Reviews, 2020-01-01, 202
Charbonnier G.;  Duchamp-Alphonse S.;  Deconinck J.-F.;  Adatte T.;  Spangenberg J.E.;  Colin C.;  Föllmi K.B.
View/Download：11/0
 
A global palaeoclimatic reconstruction for the Valanginian based on clay mineralogical and geochemical data [期刊论文]
Earth Science Reviews, 2020-01-01, 202
Charbonnier G.;  Duchamp-Alphonse S.;  Deconinck J.-F.;  Adatte T.;  Spangenberg J.E.;  Colin C.;  Föllmi K.B.
View/Download：2/0
 
Climatic and palaeoceanographic changes during the Pliensbachian (Early Jurassic) inferred from clay mineralogy and stable isotope (C-O) geochemistry (NW Europe) [期刊论文]
Global and Planetary Change, 2017-01-01, 149
Bougeault C.;  Pellenard P.;  Deconinck J.-F.;  Hesselbo S.P.;  Dommergues J.-L.;  Bruneau L.;  Cocquerez T.;  Laffont R.;  Huret E.;  Thibault N.
View/Download：43/0
 
Clay mineralogical and geochemical expressions of the "Late Campanian Event" in the Aquitaine and Paris basins (France): Palaeoenvironmental implications [期刊论文]
Palaeogeography, Palaeoclimatology, Palaeoecology, 2016-01-01, 447
Chenot E.;  Pellenard P.;  Martinez M.;  Deconinck J.-F.;  Amiotte-Suchet P.;  Thibault N.;  Bruneau L.;  Cocquerez T.;  Laffont R.;  Pucéat E.;  Robaszynski F.
View/Download：40/0
 
Astrochronology of the Valanginian-Hauterivian stages (Early Cretaceous): Chronological relationships between the Paraná-Etendeka large igneous province and the Weissert and the Faraoni events [期刊论文]
Global and Planetary Change, 2015-01-01, 131
Martinez M.;  Deconinck J.-F.;  Pellenard P.;  Riquier L.;  Company M.;  Reboulet S.;  Moiroud M.
View/Download：12/0
 
Astrochronology of the Valanginian Stage from reference sections (Vocontian Basin, France) and palaeoenvironmental implications for the Weissert Event [期刊论文]
Palaeogeography, Palaeoclimatology, Palaeoecology, 2013-01-01, 376
Martinez M.;  Deconinck J.-F.;  Pellenard P.;  Reboulet S.;  Riquier L.
View/Download：24/0
 

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