Ivor

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F06%3A00017210" target="_blank" >RIV/00216224:14310/06:00017210 - 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

Ivorian

Popis výsledku v původním jazyce

S e Ivorian Substage is the upper division of the Tournaisian. Its base, emended in this paper, corresponds to the fi rst appearance of the conodont Polygnathus communis carina in the Yvoir railway station section. Its top is defi ned by the base of theMoliniacian Substage which corresponds now to the base of the Viséan. S e Ivorian is characterized by a rich and diversifi ed conodont fauna throughout and by a diversifi cation of the foraminifers in its upper part. It is therefore very well zoned and precisely correlated across the Franco-Belgian Basin and beyond. Its upper boundary is marked by a drastic reduction of the conodont fauna and the disappearance of selected Tournaisian foraminiferal taxa. Ivorian sedimentation refl ects the evolution of the Namur-Dinant Basin from a homoclinal ramp in the early Tournaisian to a broad shelf of regional extent in the late Tournaisian. Waulsortian buildups started growing in the distal part of the ramp during early Ivorian and formed a disco

Název v anglickém jazyce

Ivorian

Popis výsledku anglicky

S e Ivorian Substage is the upper division of the Tournaisian. Its base, emended in this paper, corresponds to the fi rst appearance of the conodont Polygnathus communis carina in the Yvoir railway station section. Its top is defi ned by the base of theMoliniacian Substage which corresponds now to the base of the Viséan. S e Ivorian is characterized by a rich and diversifi ed conodont fauna throughout and by a diversifi cation of the foraminifers in its upper part. It is therefore very well zoned and precisely correlated across the Franco-Belgian Basin and beyond. Its upper boundary is marked by a drastic reduction of the conodont fauna and the disappearance of selected Tournaisian foraminiferal taxa. Ivorian sedimentation refl ects the evolution of the Namur-Dinant Basin from a homoclinal ramp in the early Tournaisian to a broad shelf of regional extent in the late Tournaisian. Waulsortian buildups started growing in the distal part of the ramp during early Ivorian and formed a disco

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

2006

Kód důvěrnosti údajů

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

Název periodika

Geologica Belgica

ISSN

1374-8505

e-ISSN

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Svazek periodika

9

Číslo periodika v rámci svazku

1/2

Stát vydavatele periodika

BE - Belgické království

Počet stran výsledku

6

Strana od-do

117-122

Kód UT WoS článku

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EID výsledku v databázi Scopus

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