The radioscopically constrained Viséan onset of turbidites in the Moravian-Silesian part of the Rhenohercynian foreland basin (Central European Variscides)
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F18%3A00000005" target="_blank" >RIV/00025798:_____/18:00000005 - isvavai.cz</a>
Result on the web
<a href="https://link.springer.com/epdf/10.1007/s00531-017-1524-3?author_access_token=mwmHxTpEU1Fi1gI6sAbokfe4RwlQNchNByi7wbcMAY5xrUM8nQOOiNHnafLY0g1KSZyYUSwbV-J279TdQ9a2QF6AHv92labzFd7S1QFBYtVkYfYO1GjJ-LpqAv03MEcuwNrFYjY1fp-9UJr_lc2EUw%3D%3D" target="_blank" >https://link.springer.com/epdf/10.1007/s00531-017-1524-3?author_access_token=mwmHxTpEU1Fi1gI6sAbokfe4RwlQNchNByi7wbcMAY5xrUM8nQOOiNHnafLY0g1KSZyYUSwbV-J279TdQ9a2QF6AHv92labzFd7S1QFBYtVkYfYO1GjJ-LpqAv03MEcuwNrFYjY1fp-9UJr_lc2EUw%3D%3D</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s00531-017-1524-3" target="_blank" >10.1007/s00531-017-1524-3</a>
Alternative languages
Result language
angličtina
Original language name
The radioscopically constrained Viséan onset of turbidites in the Moravian-Silesian part of the Rhenohercynian foreland basin (Central European Variscides)
Original language description
The Březina Formation represents the initiation of siliciclastic flysch turbidite sedimentation at the eastern margin of Bohemian Massif or within the Rhenohercynian foreland basin. Its deposition started after drowning of the Devonian carbonate platform during Viséan (Mississippian) times, resulting in a significant interval of black siliceous shale and variegated fosiliferous shale deposition in a starved basin. Near the top of the Březina Formation an acidic volcanoclastic layer (tuff) of rhyolitic composition has been dated with high precision U-Pb zircon chemical abrasion isotope dilution method at 337.73 ± 0.16 Ma. This new radiometric age correlates to the previously inferred stratigraphic age of the locality and the current calibration of the Early Carboniferous geologic time scale. Shales of the Březina Formation pass gradually upwards into the siliciclastics of the Rozstání Formation of the Drahany Culm Facies. Thus our new age offers one of the few available radioisotopic constraints on the time of onset of siliciclastic flysch turbidites in the Rheno-Hercynian foreland basin of the European Variscides.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10505 - Geology
Result continuities
Project
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Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2018
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
International Journal of Earth Sciences
ISSN
1437-3254
e-ISSN
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Volume of the periodical
107
Issue of the periodical within the volume
2
Country of publishing house
DE - GERMANY
Number of pages
17
Pages from-to
711-727
UT code for WoS article
000425001400019
EID of the result in the Scopus database
2-s2.0-85027974611