FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W995077265> ?p ?o ?g. }

• W995077265 endingPage "188" @default.
• W995077265 startingPage "139" @default.
• W995077265 abstract "Biostratygrafia i warunki paleośrodowiskowe najmlodszych osadow plaszczowiny magurskiej na wschod od Skawy w oparciu o nannoplankton wapienny (polskie Karpaty fliszowe)The Magura Nappe is the largest and southernmost tectonic unit of the Western Outer Caipathians and differ in lithofacies development from the Middle and Marginal groups of units. The age studies of the youngest deposits of the Magura Nappe play an important role in understanding the tectogenesis of the Outer Carpathians. The aim of this work was to find the litho- and biostratigraphic correlation with the more external units. For this purpose the youngest deposits from selected sections of the Magura Nappe located east of the Skawa River, were chosen. For the lower limit of the youngest sediments, Middle/Upper Eocene variegated shales with Reticulophragmium amplectens Grzybowski were taken. The analysis of nannoplankton assemblages enable to establish the age of these deposits which varies from Middle Eocene (NP15) up to Upper Oligocene (NP25) and Lower Miocene (NN2). The Eocene/Oligocene boundary lies within the NP21 nanno-zone and was found in the Krynica Zone within the Globigerina Marls (Leluchow section), in the Raca Zone within Poprad Sandstone Mbr of the Magura Fm. and in the Siary Zone within supra-Magura (Budzow) Beds (Budzow section), Wątkowa Sandstone (Ropica and Malastow sections) and within Zembrzyce (sub-Magura) Beds (Folusz section). In the Raca and Krynica zones the youngest - Upper Oligocene deposits from the studied sections belong to the Malcov Fm., whereas in the Siary Zone they belong to the supra-Magura (Budzow) Beds. The age of the Malcov Fm. was determined as NP24 in Leluchow and as NP25 in the Nowy Sącz I borehole, whereas the Budzow Beds belong to zone NP24. The youngest deposits so far described from the Magura Nappe belong to the Zawada Fm. whose age was determined as NN2. In the Polish part of the Bystrica Zone deposits younger than NP18, have so far not been found. The analysis of autochtonous nannoplankton assemblages from the Magura Basin enable to follow the palaeoecological changes in the Magura Basin, both in regional and global sense, from Late Eocene through Oligocene. The global changes are the drop of the water temperature accompanied by the progressing eutrophication of the Magura Basin. Further events were also recorded in zone NP23. The assemblage of this zone was characterised by the presence of species which are believed to be indicative of brackish water and restricted to the Paratethys region." @default.
• W995077265 created "2016-06-24" @default.
• W995077265 creator A5004636460 @default.
• W995077265 date "2001-01-01" @default.
• W995077265 modified "2023-09-23" @default.
• W995077265 title "The nannofossil biostratigraphy of the youngest deposits of the Magura Nappe (East of the Skawa river, Polish Flysch Carpathians)" @default.
• W995077265 hasPublicationYear "2001" @default.
• W995077265 type Work @default.
• W995077265 sameAs 995077265 @default.
• W995077265 citedByCount "24" @default.
• W995077265 countsByYear W9950772652012 @default.
• W995077265 countsByYear W9950772652014 @default.
• W995077265 countsByYear W9950772652015 @default.
• W995077265 countsByYear W9950772652016 @default.
• W995077265 countsByYear W9950772652017 @default.
• W995077265 countsByYear W9950772652018 @default.
• W995077265 crossrefType "journal-article" @default.
• W995077265 hasAuthorship W995077265A5004636460 @default.
• W995077265 hasConcept C109007969 @default.
• W995077265 hasConcept C127313418 @default.
• W995077265 hasConcept C151730666 @default.
• W995077265 hasConcept C153220577 @default.
• W995077265 hasConcept C17409809 @default.
• W995077265 hasConcept C2779452743 @default.
• W995077265 hasConcept C61721801 @default.
• W995077265 hasConcept C73707237 @default.
• W995077265 hasConcept C77928131 @default.
• W995077265 hasConcept C92927620 @default.
• W995077265 hasConceptScore W995077265C109007969 @default.
• W995077265 hasConceptScore W995077265C127313418 @default.
• W995077265 hasConceptScore W995077265C151730666 @default.
• W995077265 hasConceptScore W995077265C153220577 @default.
• W995077265 hasConceptScore W995077265C17409809 @default.
• W995077265 hasConceptScore W995077265C2779452743 @default.
• W995077265 hasConceptScore W995077265C61721801 @default.
• W995077265 hasConceptScore W995077265C73707237 @default.
• W995077265 hasConceptScore W995077265C77928131 @default.
• W995077265 hasConceptScore W995077265C92927620 @default.
• W995077265 hasIssue "3" @default.
• W995077265 hasLocation W9950772651 @default.
• W995077265 hasOpenAccess W995077265 @default.
• W995077265 hasPrimaryLocation W9950772651 @default.
• W995077265 hasRelatedWork W1434647897 @default.
• W995077265 hasRelatedWork W1847612085 @default.
• W995077265 hasRelatedWork W1906320655 @default.
• W995077265 hasRelatedWork W1929769252 @default.
• W995077265 hasRelatedWork W2069106497 @default.
• W995077265 hasRelatedWork W2070933681 @default.
• W995077265 hasRelatedWork W2073119996 @default.
• W995077265 hasRelatedWork W2101148475 @default.
• W995077265 hasRelatedWork W2130950244 @default.
• W995077265 hasRelatedWork W2149360730 @default.
• W995077265 hasRelatedWork W2301378540 @default.
• W995077265 hasRelatedWork W2329781224 @default.
• W995077265 hasRelatedWork W2341880108 @default.
• W995077265 hasRelatedWork W2470411697 @default.
• W995077265 hasRelatedWork W2606722627 @default.
• W995077265 hasRelatedWork W2893404196 @default.
• W995077265 hasRelatedWork W3199559604 @default.
• W995077265 hasRelatedWork W62718268 @default.
• W995077265 hasRelatedWork W765362348 @default.
• W995077265 hasRelatedWork W797002695 @default.
• W995077265 hasVolume "71" @default.
• W995077265 isParatext "false" @default.
• W995077265 isRetracted "false" @default.
• W995077265 magId "995077265" @default.
• W995077265 workType "article" @default.