FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2025011611> ?p ?o ?g. }

• W2025011611 endingPage "33" @default.
• W2025011611 startingPage "19" @default.
• W2025011611 abstract "The Yellow River presently flows into the Bohai Sea, but during the period AD 1128–1855, the river (called the Old Yellow River, OYR) flowed into the western South Yellow Sea (SYS), where the dispersal of its sediment load was controlled by the interactions among alongshore currents, waves and tides, and shelf morphology. In this study, high-resolution shallow seismic profiles, vibrocores, boreholes, and water depth data, which were obtained during geological surveys in the western SYS in recent years, are used to examine the depositional pattern and stratigraphic record related to the OYR entering the sea. Our data reveal compound clinoform morphologies (double clinoforms) – a subaerial/subaqueous delta couplet – sourced by the OYR in the western SYS. The subaerial delta comprises the currently onshore delta plain and deltafront extending to ~ 17 m in water depth, while the subaqueous delta is composed of a wide, gently inclined topset and a relatively narrow, steeply sloping foreset, stretching seaward about 160-km away from the shoreline and showing a morphological asymmetry with a generally southward deflection relative to the OYR mouth. The topset is 25–100-km wide in a shore-normal direction at water depths of 10–25 m, but is generally less than 4-m thick. The foreset is much narrower and thicker than the topset, is generally 5–30-km wide at 10–45 m water depth and is mostly 4–16-m thick with a maximum thickness of 20 m; it shows seaward-dipping internal reflectors (generally 0.3–0.5°). The rollover points (topset–foreset transition) of the subaqueous clinoform range mostly between 10 and 25 m water depth. Results of 210Pb and 137Cs geochronology indicate that maximum sediment accumulation rates (1.06 to 2.16 cm/yr) correspond to the foreset region, with much lower rates in the topset and surrounding shallow-sea regions (< 0.64 cm/yr). Marine erosion due to abandonment of the delta after 1855 and artificial dike building around the abandoned delta coast since the 1930s have impacted the sediment accumulation in the delta front in the subaerial delta and subaqueous delta. Estimates of sediment budget suggest that about 34–52% of the total load primarily from the OYR (> 97%) in AD 1128–1855 has accumulated on the subaerial delta, and that about 10–16% of the total load on the subaqueous delta. Our data also reveal that the subaqueous delta related to the OYR is underlain by a large-scale clinoform (broadly confined to ~ 2.5–9.8 cal kyr BP in age) as thick as 4–13 m with seaward-dipping lower angled (< 0.3°) internal reflectors in comparison to those in the overlying foreset deposits. Energetic marine hydrodynamics (waves, tides, and alongshore coastal-currents) and sufficient sediment supply from the OYR are interpreted to be responsible for the across-shelf subaqueous delta morphology." @default.
• W2025011611 created "2016-06-24" @default.
• W2025011611 creator A5000505099 @default.
• W2025011611 creator A5008717103 @default.
• W2025011611 creator A5011443221 @default.
• W2025011611 creator A5039565674 @default.
• W2025011611 creator A5039915214 @default.
• W2025011611 creator A5047050734 @default.
• W2025011611 date "2013-10-01" @default.
• W2025011611 modified "2023-10-06" @default.
• W2025011611 title "Subaqueous deltaic formation of the Old Yellow River (AD 1128–1855) on the western South Yellow Sea" @default.
• W2025011611 cites W1721554464 @default.
• W2025011611 cites W1973186736 @default.
• W2025011611 cites W1973935658 @default.
• W2025011611 cites W1974506265 @default.
• W2025011611 cites W1974579278 @default.
• W2025011611 cites W1975298088 @default.
• W2025011611 cites W1976626759 @default.
• W2025011611 cites W1983325553 @default.
• W2025011611 cites W1990310311 @default.
• W2025011611 cites W1993672360 @default.
• W2025011611 cites W2002009925 @default.
• W2025011611 cites W2005748695 @default.
• W2025011611 cites W2013147808 @default.
• W2025011611 cites W2020113633 @default.
• W2025011611 cites W2024667580 @default.
• W2025011611 cites W2032475257 @default.
• W2025011611 cites W2034705058 @default.
• W2025011611 cites W2035681393 @default.
• W2025011611 cites W2036529436 @default.
• W2025011611 cites W2037155954 @default.
• W2025011611 cites W2040975251 @default.
• W2025011611 cites W2041158780 @default.
• W2025011611 cites W2049143995 @default.
• W2025011611 cites W2050915780 @default.
• W2025011611 cites W2060995966 @default.
• W2025011611 cites W2063128565 @default.
• W2025011611 cites W2065123136 @default.
• W2025011611 cites W2066148746 @default.
• W2025011611 cites W2067499258 @default.
• W2025011611 cites W2073930762 @default.
• W2025011611 cites W2082416161 @default.
• W2025011611 cites W2086528171 @default.
• W2025011611 cites W2088171225 @default.
• W2025011611 cites W2089036002 @default.
• W2025011611 cites W2099328271 @default.
• W2025011611 cites W2120686284 @default.
• W2025011611 cites W2121673537 @default.
• W2025011611 cites W2146634530 @default.
• W2025011611 cites W2149765269 @default.
• W2025011611 cites W2151331038 @default.
• W2025011611 cites W2156128994 @default.
• W2025011611 cites W2169733412 @default.
• W2025011611 cites W2329998470 @default.
• W2025011611 cites W257504522 @default.
• W2025011611 cites W4376453514 @default.
• W2025011611 cites W2979042038 @default.
• W2025011611 doi "https://doi.org/10.1016/j.margeo.2013.07.003" @default.
• W2025011611 hasPublicationYear "2013" @default.
• W2025011611 type Work @default.
• W2025011611 sameAs 2025011611 @default.
• W2025011611 citedByCount "45" @default.
• W2025011611 countsByYear W20250116112014 @default.
• W2025011611 countsByYear W20250116112015 @default.
• W2025011611 countsByYear W20250116112016 @default.
• W2025011611 countsByYear W20250116112017 @default.
• W2025011611 countsByYear W20250116112018 @default.
• W2025011611 countsByYear W20250116112019 @default.
• W2025011611 countsByYear W20250116112020 @default.
• W2025011611 countsByYear W20250116112021 @default.
• W2025011611 countsByYear W20250116112022 @default.
• W2025011611 countsByYear W20250116112023 @default.
• W2025011611 crossrefType "journal-article" @default.
• W2025011611 hasAuthorship W2025011611A5000505099 @default.
• W2025011611 hasAuthorship W2025011611A5008717103 @default.
• W2025011611 hasAuthorship W2025011611A5011443221 @default.
• W2025011611 hasAuthorship W2025011611A5039565674 @default.
• W2025011611 hasAuthorship W2025011611A5039915214 @default.
• W2025011611 hasAuthorship W2025011611A5047050734 @default.
• W2025011611 hasConcept C109007969 @default.
• W2025011611 hasConcept C111368507 @default.
• W2025011611 hasConcept C114793014 @default.
• W2025011611 hasConcept C126753816 @default.
• W2025011611 hasConcept C127313418 @default.
• W2025011611 hasConcept C127413603 @default.
• W2025011611 hasConcept C135114317 @default.
• W2025011611 hasConcept C146978453 @default.
• W2025011611 hasConcept C151730666 @default.
• W2025011611 hasConcept C152382732 @default.
• W2025011611 hasConcept C5072461 @default.
• W2025011611 hasConcept C74501621 @default.
• W2025011611 hasConcept C84983702 @default.
• W2025011611 hasConceptScore W2025011611C109007969 @default.
• W2025011611 hasConceptScore W2025011611C111368507 @default.
• W2025011611 hasConceptScore W2025011611C114793014 @default.
• W2025011611 hasConceptScore W2025011611C126753816 @default.
• W2025011611 hasConceptScore W2025011611C127313418 @default.
• W2025011611 hasConceptScore W2025011611C127413603 @default.

• next