Matches in UGent Biblio for { <https://biblio.ugent.be/publication/1268703#aggregation> ?p ?o. }
Showing items 1 to 36 of
36
with 100 items per page.
- aggregation classification "A1".
- aggregation creator person.
- aggregation creator person.
- aggregation creator person.
- aggregation creator person.
- aggregation creator person.
- aggregation creator person.
- aggregation date "2010".
- aggregation format "application/pdf".
- aggregation hasFormat 1268703.bibtex.
- aggregation hasFormat 1268703.csv.
- aggregation hasFormat 1268703.dc.
- aggregation hasFormat 1268703.didl.
- aggregation hasFormat 1268703.doc.
- aggregation hasFormat 1268703.json.
- aggregation hasFormat 1268703.mets.
- aggregation hasFormat 1268703.mods.
- aggregation hasFormat 1268703.rdf.
- aggregation hasFormat 1268703.ris.
- aggregation hasFormat 1268703.txt.
- aggregation hasFormat 1268703.xls.
- aggregation hasFormat 1268703.yaml.
- aggregation isPartOf urn:issn:0016-7746.
- aggregation language "eng".
- aggregation rights "I have transferred the copyright for this publication to the publisher".
- aggregation subject "Earth and Environmental Sciences".
- aggregation title "The timing of aeolian events near archaeological settlements around Heidebos (Moervaart area, N Belgium)".
- aggregation abstract "At the locality of Heidebos (Moervaart area, N Flanders, Belgium), a sedimentary core was taken in the Maldegem-Stekene coversand ridge and dated using optically stimulated luminescence (OSL). The study aimed at contributing to an improved understanding of the evolution of the physical landscape around archaeological settlements in this area. The core comprised a 7 m thick series of laminated and massive aeolian sands, in which several organic layers were intercalated. From this sequence, 11 samples were collected for quartz-based SAR-OSL dating; an internally consistent dataset was obtained. The ages of the lowermost 1 m of the sedimentary sequence (15.5±1.1 ka and 17.3±1.3 ka) imply that these sediments may represent the time-equivalent deposit of a deflation phase that occurred during the Late Pleniglacial and led to the formation of a widespread desert pavement, regionally known as the Beuningen Gravel Bed. However, a significant part of the sediments (at least 4 m) was deposited later, i.e. during the Allerød and/or the Late Dryas. As such, the results allow establishing the genesis of the coversand ridge at the Heidebos locality on the basis of direct age information. The relatively high sedimentation rate and the absence of extensive soil formation in the record reflect periods of pronounced aeolian activity and landscape instability during the Late Glacial, which provides part of the environmental framework for human occupation in the area.".
- aggregation authorList BK573743.
- aggregation endPage "186".
- aggregation issue "3-4".
- aggregation startPage "173".
- aggregation volume "89".
- aggregation aggregates 1269658.
- aggregation isDescribedBy 1268703.
- aggregation similarTo LU-1268703.