Palaeozoic Cover of the Brunovistulian Unit

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F25%3A10169782" target="_blank" >RIV/00025798:_____/25:10169782 - isvavai.cz</a>
Alternative codes found
RIV/00216224:14310/25:00143712
Result on the web
<a href="https://doi.org/https://doi.org/10.1007/978-3-031-82911-6_9" target="_blank" >https://doi.org/https://doi.org/10.1007/978-3-031-82911-6_9</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/978-3-031-82911-6_9" target="_blank" >10.1007/978-3-031-82911-6_9</a>

Result language
angličtina
Original language name
Palaeozoic Cover of the Brunovistulian Unit
Original language description
This chapter summarizes the ideas concerning the Palaeozoic geodynamic evolution of the Brunovistulian Terrane. The review distinguishes: Allochthonous units (Western Group of Nappes) and (Par)autochthonous units and focuses on the following issues: (i) sediments of the rift basin; (ii) sediments of the foreland basin; (iii) Palaeozoic igneous activity; (iv) thermal overprint and burial history; (v) palaeobiogeography; (vi) tectonic structure. The geodynamic evolution of the Brunovistulian Terrane situated from the Cambrian near the SW edge of the East European Craton is discussed within the evolution of the Rheic Ocean at the Gondwana and Laurussia interface.
Czech name
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Czech description
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Project
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Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year
2025
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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