Sedimentological study of selected profiles of excavated area B 2012.
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F14%3A00079647" target="_blank" >RIV/00216224:14310/14:00079647 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Sedimentological study of selected profiles of excavated area B 2012.
Popis výsledku v původním jazyce
Sedimentological study of fluvial deposits in the area of Mikulčice agglomeration was enabled by the new outcrop produced due to excavation of bridge No.1 Together 8 lithofacies, forming 5 depositional units, were identified. Depositional architecture ofthese units allows better understanding of the evolution of sedimentary processes in the studied area in time and space. The oldest deposits (Pleistocene in age) reveal deposition of mostly mid-channel bars and can be most probavbly connected with braided fluvial style. The capping deposits (Holocene in age) are on the other hand connected with meandering fluvial style. Fine grained overbank deposits were in the studied outcrop preserved only as an erosional relic. Point bar sediments strongly predominate in all studied sections of the outcrop. They document point bar lateral accretion due to gradual translation of the river flow.
Název v anglickém jazyce
Sedimentological study of selected profiles of excavated area B 2012.
Popis výsledku anglicky
Sedimentological study of fluvial deposits in the area of Mikulčice agglomeration was enabled by the new outcrop produced due to excavation of bridge No.1 Together 8 lithofacies, forming 5 depositional units, were identified. Depositional architecture ofthese units allows better understanding of the evolution of sedimentary processes in the studied area in time and space. The oldest deposits (Pleistocene in age) reveal deposition of mostly mid-channel bars and can be most probavbly connected with braided fluvial style. The capping deposits (Holocene in age) are on the other hand connected with meandering fluvial style. Fine grained overbank deposits were in the studied outcrop preserved only as an erosional relic. Point bar sediments strongly predominate in all studied sections of the outcrop. They document point bar lateral accretion due to gradual translation of the river flow.
Klasifikace
Druh
C - Kapitola v odborné knize
CEP obor
AC - Archeologie, antropologie, etnologie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2014
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název knihy nebo sborníku
Mikulčice river archaeology. New interdisciplinary research into bridge No. 1.
ISBN
9788086023601
Počet stran výsledku
7
Strana od-do
85-91
Počet stran knihy
147
Název nakladatele
The Institute of Archaeology of the Academy of Sciences of the Czech Republic, Brno,
Místo vydání
Brno
Kód UT WoS kapitoly
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