GeoSed - Associazione Italiana per la Geologia del Sedimentario
Dipartimento di Scienze della Terra dell'Università di Siena
Via Laterina, 8
53100 Siena
segreteria@geosed.it
Username
Password
 


Table of Contents


Vol. 9 - 2010

Vol. 8 - 2009

Vol. 7 - 2008
SP 1 - 2008

Vol. 6 - 2007
Vol. 5 - 2006
Vol. 4 - 2005
Vol. 3 - 2004
Vol. 2 - 2003
Vol. 1 - 2001-2002

Notes for Authors
(PDF - 80 kb)



GeoActa Special Publication 1 2008


Acquisto online

GeoActa
an international Journal of Earth Sciences


Massimo Zecchin1, Luca Baradello1, Giuliano Brancolini1, Federica Donda1, Federica Rizzetto2, Luigi Tosi2
1Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, OGS, Borgo Grotta Gigante 42/c, 34010 Sgonico (TS), Italy
2Istituto di Scienze Marine, Consiglio Nazionale delle Ricerche, Castello 1364/a, 30122 Venezia, Italy

Sequence stratigraphy of Holocene deposits in the offshore of Venice based o very high-resolution seismic profiles



PDF (2,6 MB)
Abstract

Very high-resolution seismic profiles allow a sequence-stratigraphic analysis of the Holocene deposits off the Venice Lagoon. The succession is bounded at the base by an unconformity (sequence boundary), well recognizable in seismic profiles, which crops out at seaward locations. In the lower part of the Holocene succession, zones showing sub-horizontal and hummocky reflectors are separated by channelized deposits, interpreted as estuarine channel fills and distributary channel-levee systems. A sharp surface, climbing landward, truncates the lower Holocene deposits. This is overlain by a prograding shallow-marine wedge, which represents the upper part of the succession. This wedge consists of a regressive shoreface-shelf system and, locally, of ebb-tidal deltas off the lagoon inlets.
The lower part of the Holocene succession is interpreted as a transgressive systems tract, deposited during the high-amplitude sea-level rise that followed the Last Glacial Maximum. A wave ravinement surface marks the marine ingression of the late transgressive phase, and is approximately coincident with the downlap surface in seismic profiles. The prograding shallow-marine wedge represents the highstand systems tract. During this latter phase, the rate of sediment supply outpaced that of creation of accommodation. The variable thickness distribution of the TST documents important changes in the stratal architecture of the Holocene deposits along both depositional strike and dip, which may be in part due to antecedent basin physiography.

Keywords: Venice, Sequence stratigraphy, Holocene, Very high-resolution seismic stratigraphy