The interpretative significance of ripple-derived sedimentary structures within an upper Neogene fluvial succession of central Poland

dc.contributor.authorMaciaszek, Piotr
dc.contributor.authorChomiak, Lilianna
dc.contributor.authorWachocki, Robert
dc.contributor.authorWidera, Marek
dc.date.accessioned2019-05-28T12:09:20Z
dc.date.available2019-05-28T12:09:20Z
dc.date.issued2019-04
dc.description.abstractSedimentary structures discussed in the present study are genetically linked to ripples that consist of pure sand or al- ternating sand and mud layers. All types of ripple-related structures, such as climbing-ripple cross-lamination and het- erolithic bedding, i.e., flaser, wavy and lenticular (nodular), have been identified for the first time in fluvial strata that have been characterised previously as commonly massive. These small-scale bedforms, produced by migrating ripples, have been documented in a fluvial channel of late Neogene age in central Poland. The abundance and co-occurrence of the structures discussed and their spatial distribution provide evidence of their formation under very low-energy conditions, when flow velocity changed markedly, but was often significantly less than 0.5 m/s. Therefore, these rip- ple-derived sedimentary structures are here recognised as typical of channel fills of an anastomosing river.pl
dc.identifier.citationGeologos, 2019, 25, 1, 1-13.pl
dc.identifier.isbn978-83-232187-4-6
dc.identifier.issn1426-8981
dc.identifier.urihttp://hdl.handle.net/10593/24625
dc.language.isoengpl
dc.publisherWydawnictwo Naukowe UAMpl
dc.rightsinfo:eu-repo/semantics/openAccesspl
dc.subjectsedimentologypl
dc.subjectdepositional structurespl
dc.subjectripplespl
dc.subjectanastomosing riverpl
dc.titleThe interpretative significance of ripple-derived sedimentary structures within an upper Neogene fluvial succession of central Polandpl
dc.typeArtykułpl

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Uniwersytet im. Adama Mickiewicza w Poznaniu
Biblioteka Uniwersytetu im. Adama Mickiewicza w Poznaniu
Ministerstwo Nauki i Szkolnictwa Wyższego