FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2010152632> ?p ?o ?g. }

• W2010152632 endingPage "315" @default.
• W2010152632 startingPage "293" @default.
• W2010152632 abstract "Tidal sand ridges are common features on modern shelves but only few examples of such preserved sand bodies are described in Pleistocene deposits. In the stratigraphic record, some sand bodies encased in shales, previously interpreted as sand ridges, have been reinterpreted as shoreface deposits. More than 5000 km of high-resolution seismic data from the East China Sea, correlated to geotechnical boreholes and shallow cores, demonstrate the potential of sand ridge preservation and allow reconstruction of the depositional history of Pleistocene fourth order (100-kyr) depositional sequences. A high subsidence rate of about 300 m/Myr allows the preservation of three elementary sedimentary facies, constitutive of a ‘motif’ which was repeated during glacio-eustatic cycles. They consist of (1) regressive marine prodeltaic prograding wedges, (2) estuarine and continental (deltaic) facies, and (3) transgressive sand ridges, similar in shape and orientation to modern sand ridges. Major discontinuities, traceable over the entire outer continental shelf along distances of hundreds of kilometers, are transgressive and regressive surfaces of marine erosion, whereas sequence boundaries formed by fluvial erosion are difficult to identify on this low-gradient shelf. Because of the asymmetry of the Pleistocene glacio-eustatic cycles, most of the preserved sedimentary record (with the exception of sand ridges) corresponds to forced regressive deposits (deposits that formed during a seaward shift of the shoreline due to relative sea-level lowering)." @default.
• W2010152632 created "2016-06-24" @default.
• W2010152632 creator A5037648185 @default.
• W2010152632 creator A5037747238 @default.
• W2010152632 creator A5051004813 @default.
• W2010152632 creator A5056625289 @default.
• W2010152632 creator A5056668080 @default.
• W2010152632 creator A5062856721 @default.
• W2010152632 creator A5070305973 @default.
• W2010152632 creator A5086758830 @default.
• W2010152632 date "2002-08-01" @default.
• W2010152632 modified "2023-10-03" @default.
• W2010152632 title "Pleistocene forced regressions and tidal sand ridges in the East China Sea" @default.
• W2010152632 cites W1013188321 @default.
• W2010152632 cites W1513727030 @default.
• W2010152632 cites W1584140374 @default.
• W2010152632 cites W1585103557 @default.
• W2010152632 cites W1971427785 @default.
• W2010152632 cites W1979582297 @default.
• W2010152632 cites W1981505987 @default.
• W2010152632 cites W1981751303 @default.
• W2010152632 cites W2001533139 @default.
• W2010152632 cites W2002439403 @default.
• W2010152632 cites W2005748695 @default.
• W2010152632 cites W2012104619 @default.
• W2010152632 cites W2021959819 @default.
• W2010152632 cites W2032076605 @default.
• W2010152632 cites W2063128565 @default.
• W2010152632 cites W2079660177 @default.
• W2010152632 cites W2079850063 @default.
• W2010152632 cites W2094597265 @default.
• W2010152632 cites W2095441582 @default.
• W2010152632 cites W2097237010 @default.
• W2010152632 cites W2101372386 @default.
• W2010152632 cites W2107899251 @default.
• W2010152632 cites W2131740309 @default.
• W2010152632 cites W2146605432 @default.
• W2010152632 cites W2154033322 @default.
• W2010152632 cites W2158818301 @default.
• W2010152632 cites W2170612740 @default.
• W2010152632 cites W2228085811 @default.
• W2010152632 cites W2498210247 @default.
• W2010152632 cites W386200796 @default.
• W2010152632 cites W4230289598 @default.
• W2010152632 cites W4231765107 @default.
• W2010152632 cites W70842357 @default.
• W2010152632 cites W944924501 @default.
• W2010152632 doi "https://doi.org/10.1016/s0025-3227(02)00446-2" @default.
• W2010152632 hasPublicationYear "2002" @default.
• W2010152632 type Work @default.
• W2010152632 sameAs 2010152632 @default.
• W2010152632 citedByCount "172" @default.
• W2010152632 countsByYear W20101526322012 @default.
• W2010152632 countsByYear W20101526322013 @default.
• W2010152632 countsByYear W20101526322014 @default.
• W2010152632 countsByYear W20101526322015 @default.
• W2010152632 countsByYear W20101526322016 @default.
• W2010152632 countsByYear W20101526322017 @default.
• W2010152632 countsByYear W20101526322018 @default.
• W2010152632 countsByYear W20101526322019 @default.
• W2010152632 countsByYear W20101526322020 @default.
• W2010152632 countsByYear W20101526322021 @default.
• W2010152632 countsByYear W20101526322022 @default.
• W2010152632 countsByYear W20101526322023 @default.
• W2010152632 crossrefType "journal-article" @default.
• W2010152632 hasAuthorship W2010152632A5037648185 @default.
• W2010152632 hasAuthorship W2010152632A5037747238 @default.
• W2010152632 hasAuthorship W2010152632A5051004813 @default.
• W2010152632 hasAuthorship W2010152632A5056625289 @default.
• W2010152632 hasAuthorship W2010152632A5056668080 @default.
• W2010152632 hasAuthorship W2010152632A5062856721 @default.
• W2010152632 hasAuthorship W2010152632A5070305973 @default.
• W2010152632 hasAuthorship W2010152632A5086758830 @default.
• W2010152632 hasConcept C109007969 @default.
• W2010152632 hasConcept C111368507 @default.
• W2010152632 hasConcept C112959462 @default.
• W2010152632 hasConcept C114793014 @default.
• W2010152632 hasConcept C126753816 @default.
• W2010152632 hasConcept C127313418 @default.
• W2010152632 hasConcept C146588470 @default.
• W2010152632 hasConcept C151730666 @default.
• W2010152632 hasConcept C184751465 @default.
• W2010152632 hasConcept C2777620812 @default.
• W2010152632 hasConcept C53570757 @default.
• W2010152632 hasConcept C6494504 @default.
• W2010152632 hasConcept C74501621 @default.
• W2010152632 hasConcept C77271252 @default.
• W2010152632 hasConceptScore W2010152632C109007969 @default.
• W2010152632 hasConceptScore W2010152632C111368507 @default.
• W2010152632 hasConceptScore W2010152632C112959462 @default.
• W2010152632 hasConceptScore W2010152632C114793014 @default.
• W2010152632 hasConceptScore W2010152632C126753816 @default.
• W2010152632 hasConceptScore W2010152632C127313418 @default.
• W2010152632 hasConceptScore W2010152632C146588470 @default.
• W2010152632 hasConceptScore W2010152632C151730666 @default.
• W2010152632 hasConceptScore W2010152632C184751465 @default.
• W2010152632 hasConceptScore W2010152632C2777620812 @default.
• W2010152632 hasConceptScore W2010152632C53570757 @default.

• next