FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2026382879> ?p ?o ?g. }

• W2026382879 endingPage "329" @default.
• W2026382879 startingPage "318" @default.
• W2026382879 abstract "High-resolution multibeam data in the central and eastern part of the Aeolian volcanic arc (Southern Tyrrhenian Sea) reveal widespread large-scale waveforms on the submarine flanks of these insular volcanoes. These features show high variability in wave parameters (wavelength of 60–1600 m and wave height of 4–200 m) and morphology (from sinuous to arcuate in plan-view, and from undulating to stepped, with very steep scarps, in cross-section), indicating that different processes, at variable spatial and temporal scale, are responsible for their genesis. By relating the morphological characters of the different waveforms and the local boundary conditions (morphological setting, regional slope gradients, sediment source and dynamics) where these features form, we were able to distinguish bedforms formed by sedimentary gravity flows from bedform-like features due to gravity instability processes. In detail, bedforms have been interpreted as coarse-grained sediment waves according to their wave parameters, geometry and texture. Bedforms are always found where the slope gradients markedly decrease to values < 4°–8°, promoting a hydraulic jump in the sedimentary gravity flow. Hence, we tested if the recognized coarse-grained sediment waves can be generated as cyclic steps by comparing their morphometric characteristics with the results of experimental evidence and numerical modeling proposed in literature. The results show that cyclic step is a reasonable interpretation for these features, and we discuss the effect of flow depth, flow concentration and discharge as governing parameters affecting their wavelength, wave height and shape." @default.
• W2026382879 created "2016-06-24" @default.
• W2026382879 creator A5034465672 @default.
• W2026382879 creator A5036697689 @default.
• W2026382879 creator A5056989072 @default.
• W2026382879 creator A5089524032 @default.
• W2026382879 date "2014-09-01" @default.
• W2026382879 modified "2023-09-27" @default.
• W2026382879 title "Large-scale seafloor waveforms on the flanks of insular volcanoes (Aeolian Archipelago, Italy), with inferences about their origin" @default.
• W2026382879 cites W1542640906 @default.
• W2026382879 cites W1645665903 @default.
• W2026382879 cites W1968676811 @default.
• W2026382879 cites W1968789454 @default.
• W2026382879 cites W1969105056 @default.
• W2026382879 cites W1976005500 @default.
• W2026382879 cites W1979489155 @default.
• W2026382879 cites W1985589137 @default.
• W2026382879 cites W1986829755 @default.
• W2026382879 cites W1995332402 @default.
• W2026382879 cites W2009724264 @default.
• W2026382879 cites W2010234309 @default.
• W2026382879 cites W2015590041 @default.
• W2026382879 cites W2024610996 @default.
• W2026382879 cites W2035364981 @default.
• W2026382879 cites W2035584098 @default.
• W2026382879 cites W2044636302 @default.
• W2026382879 cites W2048651684 @default.
• W2026382879 cites W2053404357 @default.
• W2026382879 cites W2055227112 @default.
• W2026382879 cites W2058104782 @default.
• W2026382879 cites W2059893902 @default.
• W2026382879 cites W2061420784 @default.
• W2026382879 cites W2064768212 @default.
• W2026382879 cites W2065531835 @default.
• W2026382879 cites W2071417609 @default.
• W2026382879 cites W2089564150 @default.
• W2026382879 cites W2094626307 @default.
• W2026382879 cites W2097122956 @default.
• W2026382879 cites W2104108373 @default.
• W2026382879 cites W2121756041 @default.
• W2026382879 cites W2123473142 @default.
• W2026382879 cites W2127184000 @default.
• W2026382879 cites W2145576101 @default.
• W2026382879 cites W2152140986 @default.
• W2026382879 cites W2152391117 @default.
• W2026382879 cites W2156945129 @default.
• W2026382879 cites W2164024030 @default.
• W2026382879 cites W2169427097 @default.
• W2026382879 cites W2328748045 @default.
• W2026382879 cites W2401423790 @default.
• W2026382879 cites W2409427043 @default.
• W2026382879 doi "https://doi.org/10.1016/j.margeo.2014.06.007" @default.
• W2026382879 hasPublicationYear "2014" @default.
• W2026382879 type Work @default.
• W2026382879 sameAs 2026382879 @default.
• W2026382879 citedByCount "34" @default.
• W2026382879 countsByYear W20263828792014 @default.
• W2026382879 countsByYear W20263828792015 @default.
• W2026382879 countsByYear W20263828792016 @default.
• W2026382879 countsByYear W20263828792017 @default.
• W2026382879 countsByYear W20263828792018 @default.
• W2026382879 countsByYear W20263828792019 @default.
• W2026382879 countsByYear W20263828792020 @default.
• W2026382879 countsByYear W20263828792021 @default.
• W2026382879 countsByYear W20263828792022 @default.
• W2026382879 countsByYear W20263828792023 @default.
• W2026382879 crossrefType "journal-article" @default.
• W2026382879 hasAuthorship W2026382879A5034465672 @default.
• W2026382879 hasAuthorship W2026382879A5036697689 @default.
• W2026382879 hasAuthorship W2026382879A5056989072 @default.
• W2026382879 hasAuthorship W2026382879A5089524032 @default.
• W2026382879 hasConcept C111368507 @default.
• W2026382879 hasConcept C114793014 @default.
• W2026382879 hasConcept C117485682 @default.
• W2026382879 hasConcept C120806208 @default.
• W2026382879 hasConcept C121332964 @default.
• W2026382879 hasConcept C127313418 @default.
• W2026382879 hasConcept C151730666 @default.
• W2026382879 hasConcept C165801399 @default.
• W2026382879 hasConcept C166528214 @default.
• W2026382879 hasConcept C174943157 @default.
• W2026382879 hasConcept C180093795 @default.
• W2026382879 hasConcept C2524010 @default.
• W2026382879 hasConcept C25924097 @default.
• W2026382879 hasConcept C2779599953 @default.
• W2026382879 hasConcept C2816523 @default.
• W2026382879 hasConcept C33923547 @default.
• W2026382879 hasConcept C38349280 @default.
• W2026382879 hasConcept C62520636 @default.
• W2026382879 hasConcept C6494504 @default.
• W2026382879 hasConcept C65589250 @default.
• W2026382879 hasConcept C74532950 @default.
• W2026382879 hasConcept C8058405 @default.
• W2026382879 hasConceptScore W2026382879C111368507 @default.
• W2026382879 hasConceptScore W2026382879C114793014 @default.
• W2026382879 hasConceptScore W2026382879C117485682 @default.
• W2026382879 hasConceptScore W2026382879C120806208 @default.
• W2026382879 hasConceptScore W2026382879C121332964 @default.

• next