A sedimentary model of the Brussels Sands, Eocene, Belgium
New observations in the central Belgian Brussels Sands (transition Lower to Middle Eocene) allow to build a consistent model of the sedimentary processes and facies relationships of the deposit. The Brussels Sands fill a 120 km long and 40 km wide lowstand complex valley incision, correlated with the Yp10 50.0 Ma global lowstand. A marine transgression penetrated into the incised valleys transforming them first into estuaries and then into a tidal marine embayment. The sediment fill has a highstand signature. Filling started at the western bank, probably fed by a continuous coastal drift infer... Mehr ...
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Dokumenttyp: | Artikel |
Erscheinungsdatum: | 2011 |
Sprache: | Englisch |
Permalink: | https://search.fid-benelux.de/Record/base-26605435 |
Datenquelle: | BASE; Originalkatalog |
Powered By: | BASE |
Link(s) : | https://www.vliz.be/imisdocs/publications/267364.pdf |