Soft-sediment deformation structures in Lower Badenian (Middle Miocene) foreshore sands and their trigger mechanism (Carpathian Foredeep Basin, Czech Republic).

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F14%3A00074239" target="_blank" >RIV/00216224:14310/14:00074239 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Soft-sediment deformation structures in Lower Badenian (Middle Miocene) foreshore sands and their trigger mechanism (Carpathian Foredeep Basin, Czech Republic).

Popis výsledku v původním jazyce

Soft-sediment deformation structures have been recently recognized within Lower Badenian deposits of the Carpathian Foredeep in the outcrop near Oslavany (Moravia, Czech Republic). The deformed unit is sandwiched between undeformed foreshore deposits. The lithology (medium to fine, fine and very fine grained sands and silty sands) of both the deformed and the undeformed units is very similar. The deformation structures have been grouped into two categories, i.e. contorted and intruded. The contorted structures consist of convolute folds, contorted lamina sets and pillow-shaped structures. Cusps, dish and pillar structures, and sandy flame structures represent the intruded structures. The deformation mechanism is interpreted to be due to liquefaction/fluidization, and the seismic activity in the area under study is assumed to have been the trigger mechanism.

Název v anglickém jazyce

Soft-sediment deformation structures in Lower Badenian (Middle Miocene) foreshore sands and their trigger mechanism (Carpathian Foredeep Basin, Czech Republic).

Popis výsledku anglicky

Soft-sediment deformation structures have been recently recognized within Lower Badenian deposits of the Carpathian Foredeep in the outcrop near Oslavany (Moravia, Czech Republic). The deformed unit is sandwiched between undeformed foreshore deposits. The lithology (medium to fine, fine and very fine grained sands and silty sands) of both the deformed and the undeformed units is very similar. The deformation structures have been grouped into two categories, i.e. contorted and intruded. The contorted structures consist of convolute folds, contorted lamina sets and pillow-shaped structures. Cusps, dish and pillar structures, and sandy flame structures represent the intruded structures. The deformation mechanism is interpreted to be due to liquefaction/fluidization, and the seismic activity in the area under study is assumed to have been the trigger mechanism.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/GA205%2F09%2F0103" target="_blank" >GA205/09/0103: Mělkovodní ekosystémy středního miocénu Centrální Paratethydy: Sukcese a interakce anorganické a organické složky ekosystémů</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2014

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Austrian Journal of Earth Sciences

ISSN

0251-7493

e-ISSN

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Svazek periodika

107

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

AT - Rakouská republika

Počet stran výsledku

14

Strana od-do

23-36

Kód UT WoS článku

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EID výsledku v databázi Scopus

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