Matches in SemOpenAlex for { <https://semopenalex.org/work/W2081973407> ?p ?o ?g. }
- W2081973407 endingPage "1359" @default.
- W2081973407 startingPage "1343" @default.
- W2081973407 abstract "Abstract The southern portion of the Venice lagoon contains a relatively thick (up to 20 m) Holocene sedimentary body that represents a detailed record of the formation and evolution of the lagoon. New very high-resolution (VHR) seismic profiles provided a detailed investigation on depositional geometries, internal bounding surfaces and stratal relationships. These informations, combined with core analysis, allowed the identification of large- to medium-scale sedimentary structures (e.g. dunes, point bars), the corresponding sedimentary environment, and of retrogradational and progradational trends. In addition, the availability of dense seismic network produced a 3D reconstruction of the southern lagoon and the recognition of the along-strike and dip variability of the stratal architecture. Three main seismic units (H1–H3), separated by key stratal surfaces (S1-S3), form the Holocene succession in the southern Venice lagoon. This succession is bounded at the base by the Pleistocene/Holocene boundary (the surface S1), which consists of a surface of subaerial exposure locally subjected to river incision. The lower part of the Holocene succession (up to 13 m thick) consists of incised valley fills passing upward into lagoon and then shallow-marine sediments (Unit H1), and therefore shows a deepening-upward trend and a retrogradational stacking pattern. A prograding delta and adjacent shorelines, showing internal clinoforms downlapping onto the top of Unit H1 (the surface S2), form the middle part of the Holocene succession (Unit H2, up to 7.5 m thick). Unit H2 is interpreted as a result of a regressive phase started about 6 kyr BP and continued until recent time. The upper part of the Holocene succession (Unit H3) consists of lagoonal deposits, including tidal channel and tidal and subtidal flat sediments, that abruptly overlie Unit H2. Unit H3 is thought to represent a drowning of the area primarily due to human interventions that created rivers diversion and consequent delta abandonment during historical time." @default.
- W2081973407 created "2016-06-24" @default.
- W2081973407 creator A5030823096 @default.
- W2081973407 creator A5036609051 @default.
- W2081973407 creator A5048343106 @default.
- W2081973407 creator A5053091208 @default.
- W2081973407 creator A5074094769 @default.
- W2081973407 creator A5075717038 @default.
- W2081973407 date "2009-05-01" @default.
- W2081973407 modified "2023-09-28" @default.
- W2081973407 title "Anatomy of the Holocene succession of the southern Venice lagoon revealed by very high-resolution seismic data" @default.
- W2081973407 cites W147920229 @default.
- W2081973407 cites W1964376701 @default.
- W2081973407 cites W1964965246 @default.
- W2081973407 cites W1978909173 @default.
- W2081973407 cites W1982330450 @default.
- W2081973407 cites W1984963091 @default.
- W2081973407 cites W1987348889 @default.
- W2081973407 cites W1989164119 @default.
- W2081973407 cites W1990269982 @default.
- W2081973407 cites W1997509037 @default.
- W2081973407 cites W2000624053 @default.
- W2081973407 cites W2003346513 @default.
- W2081973407 cites W2020976786 @default.
- W2081973407 cites W2022895897 @default.
- W2081973407 cites W2026583977 @default.
- W2081973407 cites W2029339755 @default.
- W2081973407 cites W2031795031 @default.
- W2081973407 cites W2043396789 @default.
- W2081973407 cites W2052138469 @default.
- W2081973407 cites W2053896428 @default.
- W2081973407 cites W2055786492 @default.
- W2081973407 cites W2059641633 @default.
- W2081973407 cites W2060874912 @default.
- W2081973407 cites W2061858157 @default.
- W2081973407 cites W2062382700 @default.
- W2081973407 cites W2062505839 @default.
- W2081973407 cites W2072744124 @default.
- W2081973407 cites W2086010209 @default.
- W2081973407 cites W2098762071 @default.
- W2081973407 cites W2099581206 @default.
- W2081973407 cites W2103647793 @default.
- W2081973407 cites W2112052262 @default.
- W2081973407 cites W2117103196 @default.
- W2081973407 cites W2124500082 @default.
- W2081973407 cites W2132272817 @default.
- W2081973407 cites W2151298887 @default.
- W2081973407 cites W2155227165 @default.
- W2081973407 cites W2160017924 @default.
- W2081973407 cites W2165471885 @default.
- W2081973407 cites W2318756332 @default.
- W2081973407 cites W2319651375 @default.
- W2081973407 cites W2327665982 @default.
- W2081973407 cites W4231765107 @default.
- W2081973407 doi "https://doi.org/10.1016/j.csr.2009.03.006" @default.
- W2081973407 hasPublicationYear "2009" @default.
- W2081973407 type Work @default.
- W2081973407 sameAs 2081973407 @default.
- W2081973407 citedByCount "74" @default.
- W2081973407 countsByYear W20819734072012 @default.
- W2081973407 countsByYear W20819734072013 @default.
- W2081973407 countsByYear W20819734072014 @default.
- W2081973407 countsByYear W20819734072015 @default.
- W2081973407 countsByYear W20819734072016 @default.
- W2081973407 countsByYear W20819734072017 @default.
- W2081973407 countsByYear W20819734072018 @default.
- W2081973407 countsByYear W20819734072019 @default.
- W2081973407 countsByYear W20819734072020 @default.
- W2081973407 countsByYear W20819734072021 @default.
- W2081973407 countsByYear W20819734072022 @default.
- W2081973407 countsByYear W20819734072023 @default.
- W2081973407 crossrefType "journal-article" @default.
- W2081973407 hasAuthorship W2081973407A5030823096 @default.
- W2081973407 hasAuthorship W2081973407A5036609051 @default.
- W2081973407 hasAuthorship W2081973407A5048343106 @default.
- W2081973407 hasAuthorship W2081973407A5053091208 @default.
- W2081973407 hasAuthorship W2081973407A5074094769 @default.
- W2081973407 hasAuthorship W2081973407A5075717038 @default.
- W2081973407 hasConcept C111368507 @default.
- W2081973407 hasConcept C127313418 @default.
- W2081973407 hasConcept C140345934 @default.
- W2081973407 hasConcept C150117547 @default.
- W2081973407 hasConcept C151730666 @default.
- W2081973407 hasConcept C18903297 @default.
- W2081973407 hasConcept C3020199158 @default.
- W2081973407 hasConcept C62649853 @default.
- W2081973407 hasConcept C86803240 @default.
- W2081973407 hasConceptScore W2081973407C111368507 @default.
- W2081973407 hasConceptScore W2081973407C127313418 @default.
- W2081973407 hasConceptScore W2081973407C140345934 @default.
- W2081973407 hasConceptScore W2081973407C150117547 @default.
- W2081973407 hasConceptScore W2081973407C151730666 @default.
- W2081973407 hasConceptScore W2081973407C18903297 @default.
- W2081973407 hasConceptScore W2081973407C3020199158 @default.
- W2081973407 hasConceptScore W2081973407C62649853 @default.
- W2081973407 hasConceptScore W2081973407C86803240 @default.
- W2081973407 hasIssue "10" @default.
- W2081973407 hasLocation W20819734071 @default.