FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1823143906> ?p ?o ?g. }

• W1823143906 endingPage "444" @default.
• W1823143906 startingPage "419" @default.
• W1823143906 abstract "The sandy deposits produced by tsunamis and liquefaction share many sedimentary features, and distinctions between the two are important in seismically active coastal zones. Both types of deposits are present in the wetlands bordering Puget Sound, where one or more earthquakes about 1100 years ago caused both tsunami flooding and sediment venting. This co-occurrence allows an examination of the resulting deposits and a comparison with tsunami and liquefaction features of modern events. Vented sediments occur at four of five wetland field localities and tsunami deposits at two. In comparison with tsunami deposits, vented sediments in this study and from other studies tend to be thicker (although they can be thin). Vented sediments also have more variable thickness at both outcrop and map scale, are associated with injected dykes and contain clasts derived from underlying deposits. Further, vented sediments tend to contain a greater variety of sedimentary structures, and these structures vary laterally over metres. Tsunami deposits compared with vented sediments are commonly thinner, fine and thin landward more consistently, have more uniform thickness on outcrop and map scales, and have the potential of containing coarser clasts, up to boulders. For both tsunami deposits and vented sediments, the availability and grain size of source material condition the characteristics of the deposit. In the cases presented in this paper, both foraminifera and diatom assemblages within tsunami deposits and vented sediments consisted of brackish and marine species, and no distinction between processes could be made based on microfossils. In summary, this study indicates a need for more careful analysis and mapping of coastal sediments associated with earthquakes to avoid misidentification of processes and misevaluation of hazards." @default.
• W1823143906 created "2016-06-24" @default.
• W1823143906 creator A5010175161 @default.
• W1823143906 creator A5068322882 @default.
• W1823143906 date "2011-07-14" @default.
• W1823143906 modified "2023-10-04" @default.
• W1823143906 title "Vented sediments and tsunami deposits in the Puget Lowland, Washington - differentiating sedimentary processes" @default.
• W1823143906 cites W1661542716 @default.
• W1823143906 cites W1969718768 @default.
• W1823143906 cites W1973124370 @default.
• W1823143906 cites W1974551969 @default.
• W1823143906 cites W1975729129 @default.
• W1823143906 cites W1976614659 @default.
• W1823143906 cites W1978118135 @default.
• W1823143906 cites W1982872535 @default.
• W1823143906 cites W1986297985 @default.
• W1823143906 cites W1987298458 @default.
• W1823143906 cites W1989321133 @default.
• W1823143906 cites W1992478227 @default.
• W1823143906 cites W1993237173 @default.
• W1823143906 cites W1995185494 @default.
• W1823143906 cites W1997757787 @default.
• W1823143906 cites W2000760299 @default.
• W1823143906 cites W2003238592 @default.
• W1823143906 cites W2007673724 @default.
• W1823143906 cites W2010681628 @default.
• W1823143906 cites W2012692867 @default.
• W1823143906 cites W2021253901 @default.
• W1823143906 cites W2024946887 @default.
• W1823143906 cites W2027831134 @default.
• W1823143906 cites W2028719423 @default.
• W1823143906 cites W2029268904 @default.
• W1823143906 cites W2034726420 @default.
• W1823143906 cites W2037154301 @default.
• W1823143906 cites W2041893233 @default.
• W1823143906 cites W2044032465 @default.
• W1823143906 cites W2046253518 @default.
• W1823143906 cites W2048972935 @default.
• W1823143906 cites W2062659097 @default.
• W1823143906 cites W2064499777 @default.
• W1823143906 cites W2065094493 @default.
• W1823143906 cites W2068324361 @default.
• W1823143906 cites W2074580567 @default.
• W1823143906 cites W2078333278 @default.
• W1823143906 cites W2083863890 @default.
• W1823143906 cites W2088420956 @default.
• W1823143906 cites W2089111480 @default.
• W1823143906 cites W2089623642 @default.
• W1823143906 cites W2090295726 @default.
• W1823143906 cites W2096114602 @default.
• W1823143906 cites W2098333110 @default.
• W1823143906 cites W2101481684 @default.
• W1823143906 cites W2105971091 @default.
• W1823143906 cites W2108403741 @default.
• W1823143906 cites W2108499009 @default.
• W1823143906 cites W2110689430 @default.
• W1823143906 cites W2126024622 @default.
• W1823143906 cites W2128430224 @default.
• W1823143906 cites W2128532705 @default.
• W1823143906 cites W2135859728 @default.
• W1823143906 cites W2138187631 @default.
• W1823143906 cites W2145634637 @default.
• W1823143906 cites W2152687163 @default.
• W1823143906 cites W2154397679 @default.
• W1823143906 cites W2157764718 @default.
• W1823143906 cites W2160713961 @default.
• W1823143906 cites W2161878657 @default.
• W1823143906 cites W2323825484 @default.
• W1823143906 cites W2496114188 @default.
• W1823143906 cites W4211135859 @default.
• W1823143906 cites W4241188518 @default.
• W1823143906 cites W4246239059 @default.
• W1823143906 cites W4254453275 @default.
• W1823143906 cites W4376848535 @default.
• W1823143906 doi "https://doi.org/10.1111/j.1365-3091.2011.01259.x" @default.
• W1823143906 hasPublicationYear "2011" @default.
• W1823143906 type Work @default.
• W1823143906 sameAs 1823143906 @default.
• W1823143906 citedByCount "22" @default.
• W1823143906 countsByYear W18231439062012 @default.
• W1823143906 countsByYear W18231439062013 @default.
• W1823143906 countsByYear W18231439062014 @default.
• W1823143906 countsByYear W18231439062015 @default.
• W1823143906 countsByYear W18231439062016 @default.
• W1823143906 countsByYear W18231439062017 @default.
• W1823143906 countsByYear W18231439062018 @default.
• W1823143906 countsByYear W18231439062020 @default.
• W1823143906 countsByYear W18231439062021 @default.
• W1823143906 countsByYear W18231439062022 @default.
• W1823143906 crossrefType "journal-article" @default.
• W1823143906 hasAuthorship W1823143906A5010175161 @default.
• W1823143906 hasAuthorship W1823143906A5068322882 @default.
• W1823143906 hasConcept C109007969 @default.
• W1823143906 hasConcept C126753816 @default.
• W1823143906 hasConcept C127313418 @default.
• W1823143906 hasConcept C134872888 @default.
• W1823143906 hasConcept C138170599 @default.
• W1823143906 hasConcept C151730666 @default.

• next