Droz, L.; Auffret, G. A.; Savoye, B.; Bourillet, Jean-Francois (1999): L'Eventail profond de la marge celtique; stratigraphie et evolution sedimentaire The Celtic deep-sea fan; stratigraphic and sedimentary evolution. Gauthier-Villars, Montrouge, France, Comptes Rendus de l'Academie des Sciences, Serie II. Sciences de la Terre et des Planetes, 328 (3), 173-180, georefid:1999-055078

Abstract:
Seismic data collected on the Celtic Fan during Sedifan cruises (European Program Enam II), stratigraphically correlated to DSDP site 400 (leg 48) show that fan deposition was initiated during the Early Miocene. It progressively extended towards the middle of the Bay of Biscay during the Plio-Quaternary. The fan includes 3 main seismic units with several channel/levee bodies disturbed by mass-movement deposits. Depocenters shifted several times, and the present-day morphology ultimately results from a last shift of detritic inputs to the Whittard System.
Coverage:
West: -8.0000 East: -1.1000 North: 48.0000 South: 43.2000
West: NaN East: NaN North: NaN South: NaN
Data access:
Provider: SEDIS Publication Catalogue
Data set link: http://sedis.iodp.org/pub-catalogue/index.php?id=1999-055078 (c.f. for more detailed metadata)
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