Ludlow Series in the Prague Synform - a progress in biostratigraphic correlation

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F13%3A00422325" target="_blank" >RIV/67985831:_____/13:00422325 - 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

Ludlow Series in the Prague Synform - a progress in biostratigraphic correlation

Popis výsledku v původním jazyce

The Ludlow Series in the Prague Synform is marked by general transition from shale-dominated Gorstian to largely carbonate sedimentation in the Ludfordian. The facies distribution and changes reflect regressive-transgressive eustatic regime combined withtectonically unstable basin settings and synsedimentary alkaline basalt volcanism. Accordingly, shallow carbonate facies that first developed near the volcanic centers is very diverse, whereas deeper environment is rather monotonous. In the past years aprogress was made to enhance biostratigraphic correlation among local facies of the Prague Synform and the global correlation of the Ludlow strata by integration of new biostratigraphic data on graptolites, conodonts and additional pelagic and benthic faunal groups. The pronounced mid-Ludfordian Lau/Kozlowskii Event was characterized by extinction among pelagic faunas. Faunal extinction coincided with major fluctuations in sea-level indicated by local unconformities associated with debr

Název v anglickém jazyce

Ludlow Series in the Prague Synform - a progress in biostratigraphic correlation

Popis výsledku anglicky

The Ludlow Series in the Prague Synform is marked by general transition from shale-dominated Gorstian to largely carbonate sedimentation in the Ludfordian. The facies distribution and changes reflect regressive-transgressive eustatic regime combined withtectonically unstable basin settings and synsedimentary alkaline basalt volcanism. Accordingly, shallow carbonate facies that first developed near the volcanic centers is very diverse, whereas deeper environment is rather monotonous. In the past years aprogress was made to enhance biostratigraphic correlation among local facies of the Prague Synform and the global correlation of the Ludlow strata by integration of new biostratigraphic data on graptolites, conodonts and additional pelagic and benthic faunal groups. The pronounced mid-Ludfordian Lau/Kozlowskii Event was characterized by extinction among pelagic faunas. Faunal extinction coincided with major fluctuations in sea-level indicated by local unconformities associated with debr

Druh

D - Stať ve sborníku

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/GA205%2F09%2F0703" target="_blank" >GA205/09/0703: Integrovaná stratigrafie mladšího siluru (ludlow-přídolí) v pražské synformě</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2013

Kód důvěrnosti údajů

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

Název statě ve sborníku

Proceedings of the 3rd IGCP 591 Annual Meeting

ISBN

978-91-86746-87-2

ISSN

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e-ISSN

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Počet stran výsledku

2

Strana od-do

297-298

Název nakladatele

Lund University

Místo vydání

Lund

Místo konání akce

Lund

Datum konání akce

9. 6. 2013

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

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