Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/9183| DC Field | Value | Language |
|---|---|---|
| dc.contributor.authorall | Bonardi, Maurizio | en |
| dc.contributor.authorall | Tosi, Luigi | en |
| dc.contributor.editorall | Marabini, F | en |
| dc.date.accessioned | 2014-12-19T23:46:02Z | en |
| dc.date.available | 2014-12-19T23:46:02Z | en |
| dc.date.issued | 1994-10-04 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/9183 | en |
| dc.description.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. | en |
| dc.language.iso | English | en |
| dc.relation.ispartof | China-Italy Bilateral Seminar on Marine Geology | en |
| dc.subject | Late-Pleistocene | en |
| dc.subject | Lower-Holocene | en |
| dc.subject | Caranto | en |
| dc.subject | overconsolidated clay level | en |
| dc.title | The Holocene-Pleistocene boundary zone in the Lagoon of Venice | en |
| dc.title.alternative | The Holocene-Pleistocene boundary zone in the Lagoon of Venice (Italy) | en |
| dc.type | Conference paper | en |
| dc.description.status | Published | en |
| dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.10. Stratigraphy | en |
| dc.description.ConferenceLocation | Qingdao, China | en |
| dc.relation.references | BONARDI M. & CARBOGNIN L. (1992): Late Quaternary sediments differentiation and characterization by EMPA-EDS mineral assemblage study. Electron Microscopy 92, Proc. of the 10th EUREM 92, Vo!. 2, p. 603, Granada. BONARDI M. & TOSI L. (1994): I sedimenti tardo-quaternari del cordone litoraneo della Laguna di Venezia: Ie sabbie. C.N.R. Istituto per lo Studio Dinamica Grandi Masse, Tech. Rep. 184, Venezia. BONARDI M. & TOSI L. (1994): Climatic and sea level fluctuations evidenced in the mineralogical composition of Late Quaternary sediments from the Venetian Littoral (Italy). Proc. of the 14th International Sedimentological Congress, Recife, Brazil, E5. BONARDI M. & TOSI L. (1994): Effects of Late Quaternary climatic changes on an exposed clay layer in the Lagoon of Venice (Italy). Proc. of the 14th International Sedimentological Congress, Recife, Brazil, D17. GATTO P. & P REVIATELLO P. (1974): Significato stratigrafico, comportamento meccanico e distribuzione nella laguna di Venezia di un argilla sovra consolidata nota come 'caranto' . C.N.R., Istituto per lo Studio Dinamica Grandi Masse, Tech. Rep. 70, Venezia. QIN Y., ZHAO Y., CHEN L. & ZAO S., (1990): Geology of Bohai Sea. China Ocean Press, Beijing. STANLEY D. J & CHEN Z., (1993): Yangtze delta, eastern China: 1. Geometry and subsidence of Holocene depocenter. Mar. Geo!., 112: 1-11. TOSI L. (1993): Caratteristiche geotecniche del sottosuolo del litorale veneziano. C.N.R. Istituto per lo Studio della Dinamica delle Grandi Masse, Tech. Rep., 171, Venezia. TOSI L. (1994): Rapporto e prime interpretazioni sulle analisi paleontologiche condotte su campioni tardo-quaternari del sottosuolo del litorale veneziano. C.N.R. Istituto per lo Studio della Dinamica delle Grandi Masse, Tech. Rep., 182, Venezia. VISHER G. S. (1969): Grain size distributions and deposition processes. J. Sediment. Petrol. 39, 1074-1106. | en |
| dc.description.obiettivoSpecifico | 6A. Monitoraggio ambientale, sicurezza e territorio | en |
| dc.description.fulltext | open | en |
| dc.contributor.author | Bonardi, Maurizio | en |
| dc.contributor.author | Tosi, Luigi | en |
| item.openairetype | Conference paper | - |
| item.cerifentitytype | Publications | - |
| item.languageiso639-1 | en | - |
| item.grantfulltext | open | - |
| item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
| item.fulltext | With Fulltext | - |
| crisitem.classification.parent | 04. Solid Earth | - |
| Appears in Collections: | Conference materials | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| THE HOLOCENE-PLEISTOCENE BOUNDARY ZONE IN THE LAGOON OF VENICE.pdf | Main article | 5.41 MB | Adobe PDF | View/Open |
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