The interpretative significance of ripple-derived sedimentary structures within an upper Neogene fluvial succession of central Poland
dc.contributor.author | Maciaszek, Piotr | |
dc.contributor.author | Chomiak, Lilianna | |
dc.contributor.author | Wachocki, Robert | |
dc.contributor.author | Widera, Marek | |
dc.date.accessioned | 2019-05-28T12:09:20Z | |
dc.date.available | 2019-05-28T12:09:20Z | |
dc.date.issued | 2019-04 | |
dc.description.abstract | Sedimentary 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.citation | Geologos, 2019, 25, 1, 1-13. | pl |
dc.identifier.isbn | 978-83-232187-4-6 | |
dc.identifier.issn | 1426-8981 | |
dc.identifier.uri | http://hdl.handle.net/10593/24625 | |
dc.language.iso | eng | pl |
dc.publisher | Wydawnictwo Naukowe UAM | pl |
dc.rights | info:eu-repo/semantics/openAccess | pl |
dc.subject | sedimentology | pl |
dc.subject | depositional structures | pl |
dc.subject | ripples | pl |
dc.subject | anastomosing river | pl |
dc.title | The interpretative significance of ripple-derived sedimentary structures within an upper Neogene fluvial succession of central Poland | pl |
dc.type | Artykuł | pl |