FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2094594022> ?p ?o ?g. }

• W2094594022 endingPage "221" @default.
• W2094594022 startingPage "207" @default.
• W2094594022 abstract "Sediment samples were collected from a borehole in the northern South China Sea with the depositional age back to 400 ka BP, for grain size and geochemical analyses to constrain the sediment provenance and paleoenvironmental variability. Geochemical indices of Th/Sc, Ti/Nb and Th/Nb ratios suggest that the Zhujiang (Pearl River) was the main provenance of the inner shelf sediments of Hong Kong deposited during interglacial periods, whereas the locally-derived granitoids contributed significantly to the exposed inner shelf through the incision of local streams during glacial periods. Furthermore, the influence of the Zhujiang-derived sediments on the inner shelf of Hong Kong varied spatially and temporally with different sea-level changes during the past 400 kyr. Chemical weathering indices suggest hot and wet climate conditions were dominant in South China during interglacial periods of marine isotope stages (MIS) 7, 9 and 11 whereas a dry and cold paleoclimate prevailed during glacial periods of MIS 6 which accounts for weak chemical weathering and coarse-grained deposition on the inner shelf. The Holocene and last interglacial period did not see more intense chemical weathering in the Zhujiang drainage basin than other interglacial periods. Although the high resolution paleoenvironmental changes can not be easily reconstructed due to ubiquitous unconformity in the sedimentary strata and weak age controls compared to the deep sea sedimentation, the present study sheds new lights on the understanding of the transport process of the Zhujiang sediment in the deep ocean and provides a teleconnection of East Asian palaeomonsoon activity between South China, the inland and open sea areas." @default.
• W2094594022 created "2016-06-24" @default.
• W2094594022 creator A5042736130 @default.
• W2094594022 creator A5084215803 @default.
• W2094594022 creator A5084979849 @default.
• W2094594022 date "2008-02-01" @default.
• W2094594022 modified "2023-10-04" @default.
• W2094594022 title "Geochemical composition of inner shelf Quaternary sediments in the northern South China Sea with implications for provenance discrimination and paleoenvironmental reconstruction" @default.
• W2094594022 cites W1973977063 @default.
• W2094594022 cites W1976984518 @default.
• W2094594022 cites W1977209564 @default.
• W2094594022 cites W1986025435 @default.
• W2094594022 cites W1986669232 @default.
• W2094594022 cites W1988127633 @default.
• W2094594022 cites W1989193940 @default.
• W2094594022 cites W1990244657 @default.
• W2094594022 cites W1991769809 @default.
• W2094594022 cites W1996147852 @default.
• W2094594022 cites W1996932107 @default.
• W2094594022 cites W1997117037 @default.
• W2094594022 cites W1998988871 @default.
• W2094594022 cites W2001428992 @default.
• W2094594022 cites W2003767587 @default.
• W2094594022 cites W2009818246 @default.
• W2094594022 cites W2010288104 @default.
• W2094594022 cites W2012300480 @default.
• W2094594022 cites W2015720701 @default.
• W2094594022 cites W2019616124 @default.
• W2094594022 cites W2026886308 @default.
• W2094594022 cites W2028155219 @default.
• W2094594022 cites W2028436359 @default.
• W2094594022 cites W2029401070 @default.
• W2094594022 cites W2031598521 @default.
• W2094594022 cites W2034818602 @default.
• W2094594022 cites W2035988508 @default.
• W2094594022 cites W2041492958 @default.
• W2094594022 cites W2041509239 @default.
• W2094594022 cites W2049468624 @default.
• W2094594022 cites W2054440839 @default.
• W2094594022 cites W2063430850 @default.
• W2094594022 cites W2071491673 @default.
• W2094594022 cites W2073823102 @default.
• W2094594022 cites W2073930762 @default.
• W2094594022 cites W2075045172 @default.
• W2094594022 cites W2075322343 @default.
• W2094594022 cites W2075756042 @default.
• W2094594022 cites W2081011249 @default.
• W2094594022 cites W2082829558 @default.
• W2094594022 cites W2090948017 @default.
• W2094594022 cites W2094585198 @default.
• W2094594022 cites W2095262588 @default.
• W2094594022 cites W2095408941 @default.
• W2094594022 cites W2095447472 @default.
• W2094594022 cites W2103930806 @default.
• W2094594022 cites W2117350234 @default.
• W2094594022 cites W2131822677 @default.
• W2094594022 cites W2134121330 @default.
• W2094594022 cites W2158113457 @default.
• W2094594022 cites W2160940815 @default.
• W2094594022 cites W2169415627 @default.
• W2094594022 cites W2886606909 @default.
• W2094594022 cites W3150964232 @default.
• W2094594022 doi "https://doi.org/10.1016/j.gloplacha.2007.02.005" @default.
• W2094594022 hasPublicationYear "2008" @default.
• W2094594022 type Work @default.
• W2094594022 sameAs 2094594022 @default.
• W2094594022 citedByCount "57" @default.
• W2094594022 countsByYear W20945940222012 @default.
• W2094594022 countsByYear W20945940222013 @default.
• W2094594022 countsByYear W20945940222014 @default.
• W2094594022 countsByYear W20945940222016 @default.
• W2094594022 countsByYear W20945940222017 @default.
• W2094594022 countsByYear W20945940222018 @default.
• W2094594022 countsByYear W20945940222019 @default.
• W2094594022 countsByYear W20945940222020 @default.
• W2094594022 countsByYear W20945940222021 @default.
• W2094594022 countsByYear W20945940222022 @default.
• W2094594022 countsByYear W20945940222023 @default.
• W2094594022 crossrefType "journal-article" @default.
• W2094594022 hasAuthorship W2094594022A5042736130 @default.
• W2094594022 hasAuthorship W2094594022A5084215803 @default.
• W2094594022 hasAuthorship W2094594022A5084979849 @default.
• W2094594022 hasConcept C111368507 @default.
• W2094594022 hasConcept C127313418 @default.
• W2094594022 hasConcept C132651083 @default.
• W2094594022 hasConcept C151730666 @default.
• W2094594022 hasConcept C15739521 @default.
• W2094594022 hasConcept C160464908 @default.
• W2094594022 hasConcept C17409809 @default.
• W2094594022 hasConcept C184751465 @default.
• W2094594022 hasConcept C186240526 @default.
• W2094594022 hasConcept C191735495 @default.
• W2094594022 hasConcept C21790881 @default.
• W2094594022 hasConcept C2780049196 @default.
• W2094594022 hasConcept C2816523 @default.
• W2094594022 hasConcept C33683781 @default.
• W2094594022 hasConcept C40724407 @default.
• W2094594022 hasConcept C6494504 @default.

• next