Paleozoic evolution of the Moravosilesian Basin

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F00%3A00002603" target="_blank" >RIV/00216224:14310/00:00002603 - 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

Paleozoic evolution of the Moravosilesian Basin

Popis výsledku v původním jazyce

The Brunovistulian Terrane (BT) is a fragment of northern Gondwana margin regarded as a part of Avalonian group of terranes (KALVODA 1995). The lithological record of the Cambrian marine sediments may indicate the extension and rifting connected with thefragmentation of Gondwana. It is assumed that BT was amalgamated to Baltica along the TESZ in Lower Paleozoic and during the Variscan orogeny was a southern promontory of Laurussia. The Devonian extension is assumed to be connected with intraplate st resses due to the collision of the Brunovistulian promontory with Moldanubian and Armorican Superterrane. Orogeny leads to rifting at high angle to the compression direction and rifts form first near the collision site and propagate later away from it.As aconsequence, the amount of total extension and correlatively, the magnitude of the total subsidence, is commonly greatest near the suture and decreases away from it. The Moravosilesian basin bears features of both impactogen and strike-sl

Název v anglickém jazyce

Paleozoic evolution of the Moravosilesian Basin

Popis výsledku anglicky

The Brunovistulian Terrane (BT) is a fragment of northern Gondwana margin regarded as a part of Avalonian group of terranes (KALVODA 1995). The lithological record of the Cambrian marine sediments may indicate the extension and rifting connected with thefragmentation of Gondwana. It is assumed that BT was amalgamated to Baltica along the TESZ in Lower Paleozoic and during the Variscan orogeny was a southern promontory of Laurussia. The Devonian extension is assumed to be connected with intraplate st resses due to the collision of the Brunovistulian promontory with Moldanubian and Armorican Superterrane. Orogeny leads to rifting at high angle to the compression direction and rifts form first near the collision site and propagate later away from it.As aconsequence, the amount of total extension and correlatively, the magnitude of the total subsidence, is commonly greatest near the suture and decreases away from it. The Moravosilesian basin bears features of both impactogen and strike-sl

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

<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 periodika

Geolines

ISSN

1210-9606

e-ISSN

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Svazek periodika

10

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

1

Strana od-do

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Kód UT WoS článku

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EID výsledku v databázi Scopus

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