Genetic stratigraphy of Coniacian deltaic deposits of the northwestern part of the Bohemian Cretaceous Basin
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F14%3A10290397" target="_blank" >RIV/00216208:11310/14:10290397 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/67985530:_____/14:00438408
Výsledek na webu
<a href="http://dx.doi.org/10.1127/zdgg/2014/0024" target="_blank" >http://dx.doi.org/10.1127/zdgg/2014/0024</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1127/zdgg/2014/0024" target="_blank" >10.1127/zdgg/2014/0024</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Genetic stratigraphy of Coniacian deltaic deposits of the northwestern part of the Bohemian Cretaceous Basin
Popis výsledku v původním jazyce
Based on a combination of outcrop and subsurface data, this paper presents a description and interpretation of principal lithofacies and regional-scale depositional geometries in sandstones of early to middle Coniacian age in the northwestern part of theBohemian Cretaceous Basin. A depositional model of nearshore deposition presented here interprets the depositional system as dominated by coarse-grained deltas that prograded from the faulted northern basin margin, the present-day Lužice (Lausitz) FaultZone. The deltaic systems were the primary loci of clastic sediment deposition upon entering the basin, but the deposits of the delta fronts as well as part of the prodeltaic facies were further reworked by vigorous tidal currents, in particular in shallow-water settings. Steep, Gilbert-type foresets formed mainly in delta fronts that prograded into deeper water, reaching up to c. 100 m in some units. This depositional model is largely analogous to that developed by Uličný (2001) in oth
Název v anglickém jazyce
Genetic stratigraphy of Coniacian deltaic deposits of the northwestern part of the Bohemian Cretaceous Basin
Popis výsledku anglicky
Based on a combination of outcrop and subsurface data, this paper presents a description and interpretation of principal lithofacies and regional-scale depositional geometries in sandstones of early to middle Coniacian age in the northwestern part of theBohemian Cretaceous Basin. A depositional model of nearshore deposition presented here interprets the depositional system as dominated by coarse-grained deltas that prograded from the faulted northern basin margin, the present-day Lužice (Lausitz) FaultZone. The deltaic systems were the primary loci of clastic sediment deposition upon entering the basin, but the deposits of the delta fronts as well as part of the prodeltaic facies were further reworked by vigorous tidal currents, in particular in shallow-water settings. Steep, Gilbert-type foresets formed mainly in delta fronts that prograded into deeper water, reaching up to c. 100 m in some units. This depositional model is largely analogous to that developed by Uličný (2001) in oth
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
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
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 periodika
Zeitschrift der Deutschen Gesellschaft fur Geowissenschaften
ISSN
1860-1804
e-ISSN
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Svazek periodika
165
Číslo periodika v rámci svazku
4
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
29
Strana od-do
547-575
Kód UT WoS článku
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EID výsledku v databázi Scopus
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