W dniach od 2 kwietnia do 5 kwietnia 2024 r. prowadzone będą prace związane z wdrożeniem nowej wersji systemu Repozytorium UJ. Nie będzie możliwe wprowadzanie nowych informacji do repozytorium. Za utrudnienia przepraszamy.
Early Miocene age of the Stare Bystre Formation based on calcareous nannofossils (Magura Nappe, Outer Carpathians, Poland)
pl
dc.type
JournalArticle
pl
dc.description.physical
341-354, [24]
pl
dc.description.additional
Bibliogr. s. 352-354. Do publikacji dołączono 2 suplementy
pl
dc.abstract.en
The area of investigation is situated close to the contact zone between the Pieniny Klippen Belt, Krynica Subunit of the Magura Nappe and the Neogene strata of the Orava–Nowy Targ Intramontane Basin (southern Poland). In the area studied, marine deposits of the Stare Bystre Formation outcrop at the surface where they emerge from beneath freshwater and terrestrial Neogene and Quaternary deposits. Nannofossil assemblages from all samples are strongly dominated by reworked species. The Early Miocene age (NN2) of the Stare Bystre Formation has been determined on the base of the first occurrence of Sphenolithus disbelemnos after Shackleton et al. (2000). During the Late Oligocene (NP25/NN1), the frontal part of Magura Nappe was thrust northwards on to the terminal Krosno flysch basin. The northwards thrusting of the Magura Nappe was accompanied by the formation of the piggy-back basin on the Magura Nappe, filled with the synrorogenic turbidites belonging to the Zawada, Kremná and Stare Bystre formations (NN2).
pl
dc.subject.en
Outer Carpathians
pl
dc.subject.en
Magura Nappe
pl
dc.subject.en
Stare Bystre Formation
pl
dc.subject.en
nannofossils
pl
dc.subject.en
biostratigraphy
pl
dc.subject.en
reworking
pl
dc.description.volume
60
pl
dc.description.number
2
pl
dc.identifier.doi
10.7306/gq.1277
pl
dc.identifier.eissn
2082-5099
pl
dc.title.journal
Geological Quarterly
pl
dc.language.container
eng
pl
dc.affiliation
Wydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznych
pl
dc.subtype
Article
pl
dc.rights.original
CC-BY; otwarte czasopismo; ostateczna wersja wydawcy; w momencie opublikowania; 0