Applying grain-size and compositional data analysis for interpretation of the Quaternary oxbow lake sedimentation processes Eastern Great Hungarian Plain /
Grain size distribution is one of the paleoenvironmental proxies that provide insight statistical distribution of size fractions within the sediments. Multivariate statistics have been used to investigate the depositional process from the grain size dis-tribution. Still, the direct application of th...
Elmentve itt :
Szerzők: | |
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Dokumentumtípus: | Cikk |
Megjelent: |
2022
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Sorozat: | STUDIA QUATERNARIA
39 No. 2 |
Tárgyszavak: | |
doi: | 10.24425/sq.2022.140885 |
mtmt: | 33547865 |
Online Access: | http://publicatio.bibl.u-szeged.hu/29337 |
LEADER | 02055nab a2200265 i 4500 | ||
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001 | publ29337 | ||
005 | 20240118081849.0 | ||
008 | 240118s2022 hu o 0|| Angol d | ||
022 | |a 1641-5558 | ||
024 | 7 | |a 10.24425/sq.2022.140885 |2 doi | |
024 | 7 | |a 33547865 |2 mtmt | |
040 | |a SZTE Publicatio Repozitórium |b hun | ||
041 | |a Angol | ||
100 | 1 | |a Eltijani Abdelrhim | |
245 | 1 | 0 | |a Applying grain-size and compositional data analysis for interpretation of the Quaternary oxbow lake sedimentation processes |h [elektronikus dokumentum] : |b Eastern Great Hungarian Plain / |c Eltijani Abdelrhim |
260 | |c 2022 | ||
300 | |a 83-93 | ||
490 | 0 | |a STUDIA QUATERNARIA |v 39 No. 2 | |
520 | 3 | |a Grain size distribution is one of the paleoenvironmental proxies that provide insight statistical distribution of size fractions within the sediments. Multivariate statistics have been used to investigate the depositional process from the grain size dis-tribution. Still, the direct application of the standard multivariate methods is not straightforward and can yield misleading interpretations due to the compositional nature of the raw grain size data. This paper is a methodological framework for grain size data characterization through the centered log ratio transformation and euclidean data, coupled with principal component analysis, cluster analysis, and linear discriminant analysis to examine Quaternary sediments from Tovises bed in the southeast Great Hungarian Plain. These approaches provide statistically significant and sedimentologically interpretable results for both datasets. However, the details by which they supplemented the conceptual model were sig-nificantly different, and this discrepancy resulted in a different temporal model of the depositional history. | |
650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
700 | 0 | 1 | |a Molnár Dávid |e aut |
700 | 0 | 1 | |a Makó László |e aut |
700 | 0 | 1 | |a Geiger János |e aut |
700 | 0 | 1 | |a Sümegi Pál |e aut |
856 | 4 | 0 | |u http://publicatio.bibl.u-szeged.hu/29337/1/2_Eltijani.pdf |z Dokumentum-elérés |