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Late-Cenozoïc evolution of the Southern Porcupine Basin, SW off Ireland: Seismic stratigraphy and sedimentary dynamics of a passive periglacial margin

Identifier financieringsorganisatie: P102/178W1000 (Other contract id)
Periode: Januari 2000 tot December 2001
Status: Afgelopen

Thesaurustermen: Continentale randen; Fysische oceanografie; Offshore; Onderwaterakoestiek; Seismische profielen; Stratigrafie; Zijdelingse sonar
Geografische termen: ANE, Noordzee, Zuidelijke Bocht [Marine Regions]; ANE, Porcupine Seabight [Marine Regions]
 Instituten 

Instituten (2)  Top 
  • Universiteit Gent; Faculteit Wetenschappen; Vakgroep Geologie; Renard Centre of Marine Geology (RCMG), meer, coördinator
  • Vlaamse overheid; Beleidsdomein Economie, Wetenschap en Innovatie; Agentschap voor Innovatie door Wetenschap en Technologie (IWT), meer, financier

Abstract
The main interest lies in the present and past evolution of bottom currents on the Eastern slope of the Porcupine Seabight. For this study, a multitude of tools will be used:

1) Very high-resolution single-channel sparker seismics
2) Multi-channel industrial seismics
3) Very high-resolution sidescan sonar imagery
4) Swath bathymetry as well as subbottom profiling
5) Geophysical, sedimentological, micropaleontological and isotopic analyses of giant piston cores
6)This research frames within a broad cluster of international projects. The most important of these projects are situated within the Ocean Margin Cluster of the European Commission Fifth Framework Programme: GEOMOUND, ECOMOUND and STRATAGEM.

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