FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2740172373> ?p ?o ?g. }

• W2740172373 endingPage "136" @default.
• W2740172373 startingPage "118" @default.
• W2740172373 abstract "Volcanism was intense in western European basins during the Late Carboniferous–Early Permian transition, related to the late Variscan extension and associated magmatism. In the Autun Basin, explosive eruptions, expressed as highly weathered distal ashfall deposits (tonsteins), were preserved in lacustrine to swamp environments. The analysis of eleven tonsteins, confirmed as non-reworked volcanic horizons, indicates a highly explosive acidic calc-alkaline volcanism, with active volcanic centres probably linked to Massif Central or Vosges–Black Forest magmatism. New accurate CA-ID-TIMS U–Pb ages are obtained from four of these tonsteins, recorded within the lower Autunian (Igornay and Muse Fms), which defines the lower part of the Autunian stratotype in the Autun Basin. The middle part of the Igornay Fm is dated at 299.9 ± 0.38 Ma, the Lally oil-shale bed is dated at 298.91 ± 0.08 Ma and the upper part of the Muse oil-shale bed is dated between 298.05 ± 0.19 and 298.57 ± 0.16 Ma. For the first time, a numerical calibration of the regional continental Autunian stage in its stratotype is proposed, thus allowing correlation with global marine stages defined in the Urals, and highlighting a late Gzhelian/early Asselian age for the lower Autunian. The tonstein in the Lally oil-shale appears to demarcate the Carboniferous–Permian boundary within the ± 100 kyr resolution of the U-Pb ages in both the Autun and southern Uralian basins. Comparison with other European domains confirms that these new ages are consistent with well-known macrofloral assemblages, characteristic of the Autunian." @default.
• W2740172373 created "2017-08-08" @default.
• W2740172373 creator A5001616542 @default.
• W2740172373 creator A5016224782 @default.
• W2740172373 creator A5019328510 @default.
• W2740172373 creator A5024938438 @default.
• W2740172373 creator A5069457638 @default.
• W2740172373 creator A5085367456 @default.
• W2740172373 date "2017-11-01" @default.
• W2740172373 modified "2023-10-17" @default.
• W2740172373 title "High-precision U-Pb zircon ages for explosive volcanism calibrating the NW European continental Autunian stratotype" @default.
• W2740172373 cites W1585968842 @default.
• W2740172373 cites W1632042611 @default.
• W2740172373 cites W1669138304 @default.
• W2740172373 cites W1857195312 @default.
• W2740172373 cites W1964909252 @default.
• W2740172373 cites W1965281002 @default.
• W2740172373 cites W1965858395 @default.
• W2740172373 cites W1980966289 @default.
• W2740172373 cites W1981200900 @default.
• W2740172373 cites W1984019057 @default.
• W2740172373 cites W1990340825 @default.
• W2740172373 cites W1999448338 @default.
• W2740172373 cites W2000709466 @default.
• W2740172373 cites W2007056514 @default.
• W2740172373 cites W2007105153 @default.
• W2740172373 cites W2027024858 @default.
• W2740172373 cites W2027493407 @default.
• W2740172373 cites W2055417130 @default.
• W2740172373 cites W2064245639 @default.
• W2740172373 cites W2072107094 @default.
• W2740172373 cites W2072306258 @default.
• W2740172373 cites W2072405936 @default.
• W2740172373 cites W2073986814 @default.
• W2740172373 cites W2077471967 @default.
• W2740172373 cites W2081774134 @default.
• W2740172373 cites W2088320539 @default.
• W2740172373 cites W2088506630 @default.
• W2740172373 cites W2101888241 @default.
• W2740172373 cites W2104248598 @default.
• W2740172373 cites W2108971421 @default.
• W2740172373 cites W2124288485 @default.
• W2740172373 cites W2127705220 @default.
• W2740172373 cites W2137247922 @default.
• W2740172373 cites W2148467474 @default.
• W2740172373 cites W2150971507 @default.
• W2740172373 cites W2151619805 @default.
• W2740172373 cites W2153381170 @default.
• W2740172373 cites W2161267481 @default.
• W2740172373 cites W2281221565 @default.
• W2740172373 cites W2314497074 @default.
• W2740172373 cites W2315014980 @default.
• W2740172373 cites W2320129367 @default.
• W2740172373 cites W2546350922 @default.
• W2740172373 cites W2561077985 @default.
• W2740172373 cites W2567912178 @default.
• W2740172373 cites W2604672988 @default.
• W2740172373 cites W2606562385 @default.
• W2740172373 cites W2808649148 @default.
• W2740172373 cites W2973819417 @default.
• W2740172373 cites W4231852805 @default.
• W2740172373 cites W4300219558 @default.
• W2740172373 doi "https://doi.org/10.1016/j.gr.2017.07.014" @default.
• W2740172373 hasPublicationYear "2017" @default.
• W2740172373 type Work @default.
• W2740172373 sameAs 2740172373 @default.
• W2740172373 citedByCount "40" @default.
• W2740172373 countsByYear W27401723732018 @default.
• W2740172373 countsByYear W27401723732019 @default.
• W2740172373 countsByYear W27401723732020 @default.
• W2740172373 countsByYear W27401723732021 @default.
• W2740172373 countsByYear W27401723732022 @default.
• W2740172373 countsByYear W27401723732023 @default.
• W2740172373 crossrefType "journal-article" @default.
• W2740172373 hasAuthorship W2740172373A5001616542 @default.
• W2740172373 hasAuthorship W2740172373A5016224782 @default.
• W2740172373 hasAuthorship W2740172373A5019328510 @default.
• W2740172373 hasAuthorship W2740172373A5024938438 @default.
• W2740172373 hasAuthorship W2740172373A5069457638 @default.
• W2740172373 hasAuthorship W2740172373A5085367456 @default.
• W2740172373 hasConcept C109007969 @default.
• W2740172373 hasConcept C120806208 @default.
• W2740172373 hasConcept C127313418 @default.
• W2740172373 hasConcept C146357865 @default.
• W2740172373 hasConcept C149918038 @default.
• W2740172373 hasConcept C151730666 @default.
• W2740172373 hasConcept C160776313 @default.
• W2740172373 hasConcept C162973429 @default.
• W2740172373 hasConcept C17409809 @default.
• W2740172373 hasConcept C2778849375 @default.
• W2740172373 hasConcept C62476579 @default.
• W2740172373 hasConcept C77928131 @default.
• W2740172373 hasConcept C83365034 @default.
• W2740172373 hasConceptScore W2740172373C109007969 @default.
• W2740172373 hasConceptScore W2740172373C120806208 @default.
• W2740172373 hasConceptScore W2740172373C127313418 @default.
• W2740172373 hasConceptScore W2740172373C146357865 @default.
• W2740172373 hasConceptScore W2740172373C149918038 @default.

• next