LA-ICP-MS zircon ages of the Slavkov Terrane, Central Basic Belt and Basal Clastics, Brunovistulicum, Czech Republic

Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F19%3A00109560" target="_blank" >RIV/00216224:14310/19:00109560 - isvavai.cz</a>
Výsledek na webu
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Jazyk výsledku
angličtina
Název v původním jazyce
LA-ICP-MS zircon ages of the Slavkov Terrane, Central Basic Belt and Basal Clastics, Brunovistulicum, Czech Republic
Popis výsledku v původním jazyce
The 590-601 Ma age range for the Slavkov Terrane granitoids shows that their formation was coeval with that of the Thaya Terrane. The age of 740 Ma for the Central Basic Belt confirms that they formed much earlier during break-up od Rodinia. The age of the Basal Clastics show that their deposition occured around 550 Ma, i.e., after the main magmatic phase, and that nearly all clastic material was derived from local source.
Název v anglickém jazyce
LA-ICP-MS zircon ages of the Slavkov Terrane, Central Basic Belt and Basal Clastics, Brunovistulicum, Czech Republic
Popis výsledku anglicky
The 590-601 Ma age range for the Slavkov Terrane granitoids shows that their formation was coeval with that of the Thaya Terrane. The age of 740 Ma for the Central Basic Belt confirms that they formed much earlier during break-up od Rodinia. The age of the Basal Clastics show that their deposition occured around 550 Ma, i.e., after the main magmatic phase, and that nearly all clastic material was derived from local source.

Rok uplatnění
2019
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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