Evolution de la sédimentation pendant le Néogène en Méditerranée d'après les Forages JOIDES-DSDP

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Contributeur(s) Milan Universita, Istituto di Geologia e Paleontologia, Milan, Italy
Identifiant documentaire 9-5434
Identifiant OAI oai:archimer.ifremer.fr:5434
Notice source
Auteur(s): Nesteroff, Wladimir D.,Ryan, William B.f.,Hsu, Kenneth J.,Pautot, Guy,Wezel, Forese C.,Lort, Jennifer M.,Cita, Maria B.,Maync, Wolf,Stradner, Herbert,Dumitrica, Paulian
Mots clés Histoire Ifremer
Date de publication 01/01/1972
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Langue fre
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Source Pubblicazione - Milan, Universita, Istituto di Geologia e Paleontologia (Milan Universita, Istituto di Geologia e Paleontologia, Milan, Italy), 1972 , N. 125 , P. 47-62
Droits de réutilisation Milan Universita, Istituto di Geologia e Paleontologia, Milan, Italy

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Description
Examination of the GLOMAR CHALLENGER cores in the Mediterranean Sea (Leg 13) enables us to distinguish three main lithological units in the Neogene series. The lower unit is composed of blue marls with a poor, or dwarfed, fauna. The marls are of Langhian, Serravalian and Tortonian age, and are very similar to the blue marls of the same age known on land (in the Rhône basin, Vienna Basin, the Panonic Basins, etc.). This suggests that the Vindobonian Tethys received a uniform type of sedimentation. [NOT CONTROLLED OCR]
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