Brunovistulian terrane (Czech Republic, Middle European Variscides) and Lower Carboniferous Paleobiogeography

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F00%3A00002600" target="_blank" >RIV/00216224:14310/00:00002600 - 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

Brunovistulian terrane (Czech Republic, Middle European Variscides) and Lower Carboniferous Paleobiogeography

Popis výsledku v původním jazyce

The Brunovistulian Terrane was similarly as the Eastern Avalonia Terrane a part of the Panafrican (Cadomian) Gondwana margin. The lithological record of the Cambrian marine sediments may indicate the extension and rifting connected with the fragmentationof Gondwana while the faunistic record of Cambrian fauna shows close relation to Baltica (Belka et al. 1999). It is assumed that the Brunovistulian Terrane was amalgamated to the southeastern margin of Baltica and dextral translation is characteristic for its contact with northern Malopolska Terrane along the Krakow-Lubliniec Zone (Grygar, Vavro 1995). Thus the Brunovistulian Terrane was amalgamated to Baltica similarly as the Eastern Avalonia Terrane in the Lower Paleozoic, however, the Eastern Avalonian Terrane shows, contrary to the Brunovistulian Terrane, predominant sinistral translation. This differencies between the eastern and western part of the Middle European Variscides may have continued in the Upper Paleozoic. While the co

Název v anglickém jazyce

Brunovistulian terrane (Czech Republic, Middle European Variscides) and Lower Carboniferous Paleobiogeography

Popis výsledku anglicky

The Brunovistulian Terrane was similarly as the Eastern Avalonia Terrane a part of the Panafrican (Cadomian) Gondwana margin. The lithological record of the Cambrian marine sediments may indicate the extension and rifting connected with the fragmentationof Gondwana while the faunistic record of Cambrian fauna shows close relation to Baltica (Belka et al. 1999). It is assumed that the Brunovistulian Terrane was amalgamated to the southeastern margin of Baltica and dextral translation is characteristic for its contact with northern Malopolska Terrane along the Krakow-Lubliniec Zone (Grygar, Vavro 1995). Thus the Brunovistulian Terrane was amalgamated to Baltica similarly as the Eastern Avalonia Terrane in the Lower Paleozoic, however, the Eastern Avalonian Terrane shows, contrary to the Brunovistulian Terrane, predominant sinistral translation. This differencies between the eastern and western part of the Middle European Variscides may have continued in the Upper Paleozoic. While the co

Druh

D - Stať ve sborníku

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/GA205%2F99%2F1640" target="_blank" >GA205/99/1640: Paleobiogeografická evoluce foraminiferové fauny na kontaktu Gondwany a Baltiky v nejvyšším devonu a spodním karbonu</a><br>

Návaznosti

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

Rok uplatnění

2000

Kód důvěrnosti údajů

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

Název statě ve sborníku

I COngresso Ibérico de Paléontología, XVI Jornadas de la Sociedad Espanola de Paleontologia, Livro de Resumos

ISBN

972-778-026-1

ISSN

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e-ISSN

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Počet stran výsledku

1

Strana od-do

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Název nakladatele

Universidade de Evora

Místo vydání

Evora

Místo konání akce

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Datum konání akce

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Typ akce podle státní příslušnosti

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Kód UT WoS článku

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