Pleistocene terraces of the Vltava River in the Budejovice basin (Southern Bohemian Massif): New insights into sedimentary history constrained by luminescence data
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F12%3A00064394" target="_blank" >RIV/00216224:14310/12:00064394 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1016/j.geomorph.2012.04.001" target="_blank" >http://dx.doi.org/10.1016/j.geomorph.2012.04.001</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.geomorph.2012.04.001" target="_blank" >10.1016/j.geomorph.2012.04.001</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Pleistocene terraces of the Vltava River in the Budejovice basin (Southern Bohemian Massif): New insights into sedimentary history constrained by luminescence data
Popis výsledku v původním jazyce
We studied Quaternary sediments from the Budejovice basin in southern Bohemia, now being able to reconstruct the landscape formation of this area during the late Pleistocene. The main objective of this study was to map fluvial terraces of the rivers Vltava and Malse in the basin and to constrain their ages by luminescence dating. Topographic data from a high-resolution DEM in combination with lithological profiles of more than 1000 boreholes allowed identifying five terrace levels (BB 1 to BB 5) with bases ranging from 7 m below to 26 m above the recent mean water level of the Vltava River. For the lowermost terrace level BB 1, a consistent stratigraphy with ages ranging between 84.5 +/- 9.0 ka and 7.9 +/- 0.8 ka was constrained. Additionally, we obtained luminescence ages of alluvial fan and colluvial deposits, which allow us to better constrain the late Pleistocene sedimentation history of the study area.
Název v anglickém jazyce
Pleistocene terraces of the Vltava River in the Budejovice basin (Southern Bohemian Massif): New insights into sedimentary history constrained by luminescence data
Popis výsledku anglicky
We studied Quaternary sediments from the Budejovice basin in southern Bohemia, now being able to reconstruct the landscape formation of this area during the late Pleistocene. The main objective of this study was to map fluvial terraces of the rivers Vltava and Malse in the basin and to constrain their ages by luminescence dating. Topographic data from a high-resolution DEM in combination with lithological profiles of more than 1000 boreholes allowed identifying five terrace levels (BB 1 to BB 5) with bases ranging from 7 m below to 26 m above the recent mean water level of the Vltava River. For the lowermost terrace level BB 1, a consistent stratigraphy with ages ranging between 84.5 +/- 9.0 ka and 7.9 +/- 0.8 ka was constrained. Additionally, we obtained luminescence ages of alluvial fan and colluvial deposits, which allow us to better constrain the late Pleistocene sedimentation history of the study area.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2012
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Geomorphology
ISSN
0169-555X
e-ISSN
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Svazek periodika
161
Číslo periodika v rámci svazku
1
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
15
Strana od-do
58-72
Kód UT WoS článku
000305672700005
EID výsledku v databázi Scopus
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