FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2576256935> ?p ?o ?g. }

• W2576256935 endingPage "215" @default.
• W2576256935 startingPage "204" @default.
• W2576256935 abstract "There has been considerable progress in tsunami research in recent years, yet most work has been focussed on identifying and understanding the evidence of large events. This study aimed to identify the evidence of small historical tsunamis in Lyttelton Harbour, New Zealand. The study area has been inundated by multiple relatively small historical tsunamis that left atypical sedimentary evidence (no sand) or no sediment. Shallow trenches revealed discontinuous layers of small grey mud clasts at various depths across the study area, most likely transported from the nearby tidal flats. The origin of these mud clast layers was investigated using a multi-proxy approach comprising sedimentological, geochemical and diatom analyses complemented by dating from 137Cs activity profiles and historical data. Subtle variations consistent with inclusions of marine mud such as a decrease in organic content and magnetic susceptibility and increases in geochemical markers (e.g. Ca/kcps, K/kcps, K/Rb, Si/Rb and Sr/Rb) were found in the sediment profile. Variations in diatom assemblages suggesting a marine influence were also recorded at similar depths, aligning with layers of mud clasts. Using 137Cs activity profiles and historical data, these deposits were attributed to the 1960 Chile Valdivia and 1964 Alaska tsunamis, as well as a possible earlier event. Sedimentary evidence for the 2010 Chile Maule tsunami was not found at the study site, but geochemical analysis of surface samples revealed marked changes in Ca, Cl, Sr and Ti concentrations, indicative of a change from a terrestrial to marine influence. This was used to identify the landward extent of inundation by the 2010 event. Ultimately, this study shows that a broad multi-proxy analysis can distinguish even the subtle signatures of an inconspicuous deposit laid down by a small tsunami." @default.
• W2576256935 created "2017-01-26" @default.
• W2576256935 creator A5004018480 @default.
• W2576256935 creator A5010959622 @default.
• W2576256935 creator A5024006487 @default.
• W2576256935 creator A5031373819 @default.
• W2576256935 creator A5038151473 @default.
• W2576256935 creator A5089355054 @default.
• W2576256935 date "2017-03-01" @default.
• W2576256935 modified "2023-10-09" @default.
• W2576256935 title "Multi-proxy evidence for small historical tsunamis leaving little or no sedimentary record" @default.
• W2576256935 cites W1494431475 @default.
• W2576256935 cites W1892250996 @default.
• W2576256935 cites W1966801905 @default.
• W2576256935 cites W1970749732 @default.
• W2576256935 cites W1976783623 @default.
• W2576256935 cites W1977475476 @default.
• W2576256935 cites W1984879127 @default.
• W2576256935 cites W1987800877 @default.
• W2576256935 cites W1989497199 @default.
• W2576256935 cites W2002506179 @default.
• W2576256935 cites W2007765260 @default.
• W2576256935 cites W2023317688 @default.
• W2576256935 cites W2027192132 @default.
• W2576256935 cites W2028996645 @default.
• W2576256935 cites W2030376128 @default.
• W2576256935 cites W2035793502 @default.
• W2576256935 cites W2053737168 @default.
• W2576256935 cites W2053870388 @default.
• W2576256935 cites W2054737115 @default.
• W2576256935 cites W2055434757 @default.
• W2576256935 cites W2058275453 @default.
• W2576256935 cites W2061676462 @default.
• W2576256935 cites W2064760603 @default.
• W2576256935 cites W2065495362 @default.
• W2576256935 cites W2067810404 @default.
• W2576256935 cites W2071781238 @default.
• W2576256935 cites W2074580567 @default.
• W2576256935 cites W2077267127 @default.
• W2576256935 cites W2085559815 @default.
• W2576256935 cites W2087393748 @default.
• W2576256935 cites W2090194832 @default.
• W2576256935 cites W2090295726 @default.
• W2576256935 cites W2090740602 @default.
• W2576256935 cites W2090993619 @default.
• W2576256935 cites W2115333736 @default.
• W2576256935 cites W2121987620 @default.
• W2576256935 cites W2131810031 @default.
• W2576256935 cites W2159525271 @default.
• W2576256935 cites W2226236520 @default.
• W2576256935 cites W2234110652 @default.
• W2576256935 cites W2512211076 @default.
• W2576256935 cites W2560361148 @default.
• W2576256935 doi "https://doi.org/10.1016/j.margeo.2017.01.002" @default.
• W2576256935 hasPublicationYear "2017" @default.
• W2576256935 type Work @default.
• W2576256935 sameAs 2576256935 @default.
• W2576256935 citedByCount "38" @default.
• W2576256935 countsByYear W25762569352017 @default.
• W2576256935 countsByYear W25762569352018 @default.
• W2576256935 countsByYear W25762569352019 @default.
• W2576256935 countsByYear W25762569352020 @default.
• W2576256935 countsByYear W25762569352021 @default.
• W2576256935 countsByYear W25762569352022 @default.
• W2576256935 countsByYear W25762569352023 @default.
• W2576256935 crossrefType "journal-article" @default.
• W2576256935 hasAuthorship W2576256935A5004018480 @default.
• W2576256935 hasAuthorship W2576256935A5010959622 @default.
• W2576256935 hasAuthorship W2576256935A5024006487 @default.
• W2576256935 hasAuthorship W2576256935A5031373819 @default.
• W2576256935 hasAuthorship W2576256935A5038151473 @default.
• W2576256935 hasAuthorship W2576256935A5089355054 @default.
• W2576256935 hasConcept C111368507 @default.
• W2576256935 hasConcept C127313418 @default.
• W2576256935 hasConcept C138170599 @default.
• W2576256935 hasConcept C151730666 @default.
• W2576256935 hasConcept C17409809 @default.
• W2576256935 hasConcept C193539361 @default.
• W2576256935 hasConcept C2778902744 @default.
• W2576256935 hasConcept C2816523 @default.
• W2576256935 hasConcept C6494504 @default.
• W2576256935 hasConceptScore W2576256935C111368507 @default.
• W2576256935 hasConceptScore W2576256935C127313418 @default.
• W2576256935 hasConceptScore W2576256935C138170599 @default.
• W2576256935 hasConceptScore W2576256935C151730666 @default.
• W2576256935 hasConceptScore W2576256935C17409809 @default.
• W2576256935 hasConceptScore W2576256935C193539361 @default.
• W2576256935 hasConceptScore W2576256935C2778902744 @default.
• W2576256935 hasConceptScore W2576256935C2816523 @default.
• W2576256935 hasConceptScore W2576256935C6494504 @default.
• W2576256935 hasFunder F4320320435 @default.
• W2576256935 hasFunder F4320320965 @default.
• W2576256935 hasLocation W25762569351 @default.
• W2576256935 hasOpenAccess W2576256935 @default.
• W2576256935 hasPrimaryLocation W25762569351 @default.
• W2576256935 hasRelatedWork W1868012504 @default.
• W2576256935 hasRelatedWork W1958275154 @default.
• W2576256935 hasRelatedWork W1995558841 @default.

• next