DC pole | Wartość | Język |
dc.contributor.author | Brachaniec, Tomasz | - |
dc.date.accessioned | 2020-04-07T05:41:42Z | - |
dc.date.available | 2020-04-07T05:41:42Z | - |
dc.date.issued | 2018 | - |
dc.identifier.citation | "Meteoritics and Planetary Science" iss. 3 (2018), s. 505-513 | pl_PL |
dc.identifier.issn | 1945-5100 | - |
dc.identifier.uri | http://hdl.handle.net/20.500.12128/13460 | - |
dc.description.abstract | Reworking and redeposition of tektites is a highly complex and multistage
geological process including many factors. A tumbling experiment was therefore undertaken
with the aim of estimating a distance of transport that such moldavites can withstand.
Though the experiment probably did not accurately mimic natural conditions, our results
proved that moldavites can withstand considerable transport only over a distance of a few
kilometers. Observed abrasion of tektites was significant in the early stage of experimental
transport; the rate of abrasion decreased correlatively with increasing distance of transport
as usual. Overall, given the results obtained from this experimental study and their state of
preservation described in the literature, it is very likely that Polish tektites were reworked
and redeposited by rivers from the Sudetes Mountains. Based on the paleoreconstruction of
river flows, it can be assumed that the Polish tektites originated from two independent
sediment supply areas. | pl_PL |
dc.language.iso | en | pl_PL |
dc.rights | Uznanie autorstwa-Użycie niekomercyjne-Bez utworów zależnych 3.0 Polska | * |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/pl/ | * |
dc.subject | Polish tektites | pl_PL |
dc.subject | fluvial transport | pl_PL |
dc.title | An experimental model for the tektite fluvial transport based on the most distal Polish moldavite occurrences | pl_PL |
dc.type | info:eu-repo/semantics/article | pl_PL |
dc.identifier.doi | 10.1111/maps.13035 | - |
Pojawia się w kolekcji: | Artykuły (WNP)
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