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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9183

Authors: Bonardi, Maurizio
Tosi, Luigi
Title: The Holocene-Pleistocene boundary zone in the Lagoon of Venice
Other Titles: The Holocene-Pleistocene boundary zone in the Lagoon of Venice (Italy)
Editors: Marabini, F
Issue Date: 4-Oct-1994
Keywords: Late-Pleistocene
Lower-Holocene
Caranto
overconsolidated clay level
Abstract: The results of a detailed study on the sediments representative of the boundary area from the Late-Pleistocene and the Lower-Holocene sedimentations are reported. Mineralogical, granulometric and geochemical investigations have been carried out to characterize the clay-rich samples taken along the littoral bar and representative of the continental and marine sedimentations. Particular attention was devoted to the study of the overconsolidated clay layer considered to be the last continental deposit before the Holocene (Flandrian) transgression and interpreted as a paleosol.
Appears in Collections:Conference materials
04.04.10. Stratigraphy

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THE HOLOCENE-PLEISTOCENE BOUNDARY ZONE IN THE LAGOON OF VENICE.pdfMain article5.41 MBAdobe PDFView/Open


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