Compositional variations and patterns of conodont reworkinging in Late Devonian and Early Carboniferous calciturbidites (Moravia, Czech Republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F01%3A00004675" target="_blank" >RIV/00216224:14310/01:00004675 - 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

Compositional variations and patterns of conodont reworkinging in Late Devonian and Early Carboniferous calciturbidites (Moravia, Czech Republic)

Popis výsledku v původním jazyce

Compositional variations and grain-size properties of both carbonate constituents and conodonts as an alternative component group were used for interpreting the processes governing the deposition of upper Famennian and middle Tournaisian calciturbiditesin Moravia, Czech Republic. Both the composition and grain-size properties of conodont element associations showed to be markedly dependant on facies type of their host sediment. Upper Devonian calciturbidite successions deposited on flanks of wide, Moravian - Silesian carbonate platform are composed mainly of echinoderm- and peloid-rich wacke/packstones and intraclastic float/rudstones (fine-grained calciturbidites, "normal" calciturbidites with Tab Bouma sequences,debris-flow breccias) with abundanceof shelf- and shelf margin conodont taxa and epipelagic and "mesopelagic" conodonts. Upper Devonian calciturbidites deposited on slopes of volcanic sea-mounts are composed of echinoderm- and peloid-rich wacke/packstones and float/rudstone

Název v anglickém jazyce

Compositional variations and patterns of conodont reworkinging in Late Devonian and Early Carboniferous calciturbidites (Moravia, Czech Republic)

Popis výsledku anglicky

Compositional variations and grain-size properties of both carbonate constituents and conodonts as an alternative component group were used for interpreting the processes governing the deposition of upper Famennian and middle Tournaisian calciturbiditesin Moravia, Czech Republic. Both the composition and grain-size properties of conodont element associations showed to be markedly dependant on facies type of their host sediment. Upper Devonian calciturbidite successions deposited on flanks of wide, Moravian - Silesian carbonate platform are composed mainly of echinoderm- and peloid-rich wacke/packstones and intraclastic float/rudstones (fine-grained calciturbidites, "normal" calciturbidites with Tab Bouma sequences,debris-flow breccias) with abundanceof shelf- and shelf margin conodont taxa and epipelagic and "mesopelagic" conodonts. Upper Devonian calciturbidites deposited on slopes of volcanic sea-mounts are composed of echinoderm- and peloid-rich wacke/packstones and float/rudstone

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

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2001

Kód důvěrnosti údajů

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

Název periodika

Facies

ISSN

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e-ISSN

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Svazek periodika

44

Číslo periodika v rámci svazku

-

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

16

Strana od-do

211

Kód UT WoS článku

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EID výsledku v databázi Scopus

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