Matches in SemOpenAlex for { <https://semopenalex.org/work/W4296010579> ?p ?o ?g. }
- W4296010579 endingPage "270" @default.
- W4296010579 startingPage "244" @default.
- W4296010579 abstract "Abstract We present new sedimentological, petrographical, palaeontological and detrital zircon U–Pb data on late Oligocene–early Miocene sedimentary rocks of the thin‐skinned thrust belt of East Carpathians. These data were acquired to reconstruct the sedimentary routing system for two compositionally different turbidite fans made of the regionally extensive Kliwa and Fusaru formations. On the eastern margin of the Moldavides foreland basin, large low‐gradient river systems draining the East European Platform provided well‐sorted quartz‐rich sand forming deltas on wide shallow shelves and thick Kliwa submarine fans. Due to the westward subduction of a thinned continental plate, the western basin margin was characterized by short, steep‐gradient routing systems where sediment transport to deep water was mainly through hyperpycnal flows. The Getic and Bucovinian nappes of the East Carpathians and the exhumed Cretaceous–Early Palaeogene orogenic wedge fed Fusaru fans with poorly sorted lithic sand. The Fusaru fans trend northwards in the foredeep basin having an elongate depocentre, interfingering and then overlapping on the distal part of the Kliwa depositional system due to the eastward advance of the Carpathian fold‐and‐thrust belt. A smaller sediment input is supplied by southern continental areas (i.e. Moesian Platform, North Dobrogea and potentially the Balkans). In general, the sandstone interfingering between distinct basin floor fan systems is less well documented because the facies would be similar and there are not many systems that have a distinct sediment provenance like Kliwa and Fusaru systems. This case study improves the understanding of regional palaeogeography and sedimentary routing systems and provides observations relevant here or elsewhere on the interfingering turbidite fan systems." @default.
- W4296010579 created "2022-09-17" @default.
- W4296010579 creator A5010644657 @default.
- W4296010579 creator A5024995961 @default.
- W4296010579 creator A5026587715 @default.
- W4296010579 creator A5055054874 @default.
- W4296010579 creator A5059779729 @default.
- W4296010579 creator A5065495069 @default.
- W4296010579 creator A5071963155 @default.
- W4296010579 creator A5090009631 @default.
- W4296010579 date "2022-09-17" @default.
- W4296010579 modified "2023-10-16" @default.
- W4296010579 title "Provenance of Oligocene lithic and quartz arenites of the East Carpathians: Understanding sediment routing systems on compressional basin margins" @default.
- W4296010579 cites W1170163130 @default.
- W4296010579 cites W141993106 @default.
- W4296010579 cites W1599983827 @default.
- W4296010579 cites W1685029859 @default.
- W4296010579 cites W1966440077 @default.
- W4296010579 cites W1974558784 @default.
- W4296010579 cites W1975916925 @default.
- W4296010579 cites W1985936017 @default.
- W4296010579 cites W1999470607 @default.
- W4296010579 cites W2002167683 @default.
- W4296010579 cites W2018681920 @default.
- W4296010579 cites W2021329631 @default.
- W4296010579 cites W2032822918 @default.
- W4296010579 cites W2034905496 @default.
- W4296010579 cites W2036383229 @default.
- W4296010579 cites W2041734868 @default.
- W4296010579 cites W2043394534 @default.
- W4296010579 cites W2047846840 @default.
- W4296010579 cites W2049320595 @default.
- W4296010579 cites W2049705812 @default.
- W4296010579 cites W2055375154 @default.
- W4296010579 cites W2062732835 @default.
- W4296010579 cites W2068600269 @default.
- W4296010579 cites W2083456023 @default.
- W4296010579 cites W2083882007 @default.
- W4296010579 cites W2086570039 @default.
- W4296010579 cites W2088134820 @default.
- W4296010579 cites W2093369526 @default.
- W4296010579 cites W2119566872 @default.
- W4296010579 cites W2126641321 @default.
- W4296010579 cites W2165609841 @default.
- W4296010579 cites W2167293470 @default.
- W4296010579 cites W2174216460 @default.
- W4296010579 cites W2213808876 @default.
- W4296010579 cites W2214732944 @default.
- W4296010579 cites W2233230354 @default.
- W4296010579 cites W2237033176 @default.
- W4296010579 cites W2273583313 @default.
- W4296010579 cites W2311034980 @default.
- W4296010579 cites W2316858355 @default.
- W4296010579 cites W2474718127 @default.
- W4296010579 cites W2506873391 @default.
- W4296010579 cites W2510768065 @default.
- W4296010579 cites W2515871043 @default.
- W4296010579 cites W2527224219 @default.
- W4296010579 cites W2578332754 @default.
- W4296010579 cites W2605364770 @default.
- W4296010579 cites W2616254182 @default.
- W4296010579 cites W2621843496 @default.
- W4296010579 cites W2753821357 @default.
- W4296010579 cites W2761989018 @default.
- W4296010579 cites W2793718337 @default.
- W4296010579 cites W2807893319 @default.
- W4296010579 cites W2884049800 @default.
- W4296010579 cites W2889406993 @default.
- W4296010579 cites W2906700722 @default.
- W4296010579 cites W2917722911 @default.
- W4296010579 cites W2942527572 @default.
- W4296010579 cites W2965114178 @default.
- W4296010579 cites W2970359700 @default.
- W4296010579 cites W2971609132 @default.
- W4296010579 cites W2983477506 @default.
- W4296010579 cites W2992917493 @default.
- W4296010579 cites W3006193723 @default.
- W4296010579 cites W3016306793 @default.
- W4296010579 cites W3016403889 @default.
- W4296010579 cites W3025424653 @default.
- W4296010579 cites W3031649105 @default.
- W4296010579 cites W3084153055 @default.
- W4296010579 cites W3127390367 @default.
- W4296010579 cites W3135014934 @default.
- W4296010579 cites W3169343427 @default.
- W4296010579 cites W3169347214 @default.
- W4296010579 cites W3196629391 @default.
- W4296010579 cites W4210820632 @default.
- W4296010579 cites W4229981469 @default.
- W4296010579 cites W4232328127 @default.
- W4296010579 cites W4255968852 @default.
- W4296010579 cites W4302767268 @default.
- W4296010579 doi "https://doi.org/10.1111/bre.12711" @default.
- W4296010579 hasPublicationYear "2022" @default.
- W4296010579 type Work @default.
- W4296010579 citedByCount "1" @default.
- W4296010579 countsByYear W42960105792023 @default.
- W4296010579 crossrefType "journal-article" @default.