Shekarifard, Ali, Baudin, François, Seyed-Emami, Kazem, Schnyder, Johann, Laggoun-Défarge, Fatima, Riboulleau, Armelle, ...
Organic petrography and geochemical analyses have been carried out on the shales, carbonaceous shales and coals of the Shemshak Group (Upper Triassic-Middle Jurassic) from fifteen localities along...
Shekarifard, Ali, Baudin, François, Seyed-Emami, Kazem, Schnyder, Johann, Laggoun-Défarge, Fatima, Riboulleau, Armelle, ...
Organic petrography and geochemical analyses have been carried out on the shales, carbonaceous shales and coals of the Shemshak Group (Upper Triassic-Middle Jurassic) from fifteen localities along...
BAUDIN, François, MOULLADE, Michel, TRONCHETTI, Guy
Les teneurs en Carbone Organique Total (COT) des couches gargasiennes étudiées dans leur région stratotypique historique sont faibles (0,3% en moyenne), à l'exception de quelques niveaux où les...
Baudin, François, Moullade, Michel, Tronchetti, Guy
The Total Organic Carbon (TOC) content of the Gargasian strata studied in their historical stratotype area is rather low (0.3% on average). Only a few levels show TOC values approaching 1.2%. This...
Baudin, François, Moullade, Michel, Tronchetti, Guy
The Total Organic Carbon (TOC) content of the Gargasian strata studied in their historical stratotype area is rather low (0.3% on average). Only a few levels show TOC values approaching 1.2%. This...
Giraud, Fabienne, Courtinat, Bernard, Garcia, Jean-Pierre, Baudin, François, Guillocheau, François, Dromart, Gilles, ...
Blanke, R., Bouloubassi, I., Baudin, François, Lallier-Vergès, Elisabeth, Meyers, P.
La marge Sud-Est Atlantique a été le siège d'une accumulation très importante de carbone organique durant les derniers cycles climatiques : les teneurs y sont parmi les plus élevées du monde...
Blanke, R., Bouloubassi, I., Baudin, François, Lallier-Vergès, Elisabeth, Meyers, P.
La marge Sud-Est Atlantique a été le siège d'une accumulation très importante de carbone organique durant les derniers cycles climatiques : les teneurs y sont parmi les plus élevées du monde...
Blanke, Raphaël, Bouloubassi, I., Baudin, François, Lallier-Vergès, Elisabeth, Meyers, P.
La marge Sud-Est Atlantique a été le siège d'une accumulation très importante de carbone organique durant les derniers cycles climatiques : les teneurs y sont parmi les plus élevées du monde...
Blanke, Raphaël, Bouloubassi, I., Baudin, François, Lallier-Vergès, Elisabeth, Meyers, P.
La marge Sud-Est Atlantique a été le siège d'une accumulation très importante de carbone organique durant les derniers cycles climatiques : les teneurs y sont parmi les plus élevées du monde...
Baudin, François, Blanke, R., Pichevin, Laetitia, Tranier, J., Bertrand, Philippe, Disnar, Jean-Robert, ...
Classical views for the deposition of organic-rich sediments in deep-sea environments invoke two principal types of oceanographic and sedimentologic settings. The first is confined basins in which...
Baudin, François, Blanke, R., Pichevin, Laetitia, Tranier, J., Bertrand, Philippe, Disnar, Jean-Robert, ...
Classical views for the deposition of organic-rich sediments in deep-sea environments invoke two principal types of oceanographic and sedimentologic settings. The first is confined basins in which...
Baudin, François, Blanke, R., Pichevin, Laetitia, Tranier, J., Bertrand, Philippe, Disnar, Jean-Robert, ...
Classical views for the deposition of organic-rich sediments in deep-sea environments invoke two principal types of oceanographic and sedimentologic settings. The first is confined basins in which...
Baudin, François, Blanke, Raphaël, Pichevin, Laetitia, Tranier, J., Bertrand, Philippe, Disnar, Jean-Robert, ...
Classical views for the deposition of organic-rich sediments in deep-sea environments invoke two principal types of oceanographic and sedimentologic settings. The first is confined basins in which...
Baudin, François, Blanke, Raphaël, Pichevin, Laetitia, Tranier, J., Bertrand, Philippe, Disnar, Jean-Robert, ...
Classical views for the deposition of organic-rich sediments in deep-sea environments invoke two principal types of oceanographic and sedimentologic settings. The first is confined basins in which...
Baudin, François, Blanke, Raphaël, Pichevin, Laetitia, Tranier, J., Bertrand, Philippe, Disnar, Jean-Robert, ...
Classical views for the deposition of organic-rich sediments in deep-sea environments invoke two principal types of oceanographic and sedimentologic settings. The first is confined basins in which...
Baudin, François, Tribovillard, Nicolas, Laggoun-Défarge, Fatima, Lichtfouse, E., Monod, Olivier, Gardin, Silvia
The Upper Jurassic Akkuyu Formation of south-western Turkey consists of pale-coloured carbonate facies, but includes a peculiar black band' at its base. In order to characterize the depositional...
Baudin, François, Tribovillard, Nicolas, Laggoun-Défarge, Fatima, Lichtfouse, E., Monod, Olivier, Gardin, Silvia
The Upper Jurassic Akkuyu Formation of south-western Turkey consists of pale-coloured carbonate facies, but includes a peculiar black band' at its base. In order to characterize the depositional...
Lichtfouse, Eric, Chenu, Claire, Baudin, François, Leblond, Claudette, Da Silva, Martine, Béhar, Françoise, ...
A resistant soil organic residue, humin, has been analysed by solid-state 13C-NMR and pyrolysis followed by molecular and 13C determination of the pyrolysate alkane-alkene fraction. The results...
Lichtfouse, Eric, Chenu, Claire, Baudin, François, Leblond, Claudette, Da Silva, Martine, Béhar, Françoise, ...
A resistant soil organic residue, humin, has been analysed by solid-state 13C-NMR and pyrolysis followed by molecular and 13C determination of the pyrolysate alkane-alkene fraction. The results...
Resistant ultralaminae in soils (1996)
Lichtfouse, Eric, Chenu, Claire, Baudin, François
Observation of a chemically resistant organic residue from maize crop soils by transmission electron microscopy reveals the occurrence of thin laminae with 10-50 nm thickness, similar to resistant,...
Resistant ultralaminae in soils (1996)
Lichtfouse, Eric, Chenu, Claire, Baudin, François
Observation of a chemically resistant organic residue from maize crop soils by transmission electron microscopy reveals the occurrence of thin laminae with 10-50 nm thickness, similar to resistant,...