Silurian stratigraphy and paleogeography of north Gondwanan and Perunican Europe

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F03%3A00000125" target="_blank" >RIV/00025798:_____/03:00000125 - isvavai.cz</a>
Alternative codes found
RIV/00025798:_____/03:00000126
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Silurian stratigraphy and paleogeography of north Gondwanan and Perunican Europe
Original language description
The modern geographical distribution of north Gondwanan regions with Silurian sediments and faunas, shows a rather complex and disorganized picture. This apparent disorganization mainly resulted from tectonism during the Variscan Orogeny and, to a minordegree, later modifications by the Alpine Orogeny. We infer that the pre-orogenic paleogeography of the north Gondwanan Silurian featured a continuous shelf that can be divided into proximal and distal parts. The Perunica microcontinent (i.e., the resent-day Bohemian Massif) was incorporated into the Variscan orogen as terrane between the Gondwana and Baltica continents. The existence of Perunica is supported by paleomagnetic data and by the distribution of Ordovician and Silurian fossil
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Publication year
2003
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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