FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2281252973> ?p ?o ?g. }

• W2281252973 endingPage "351" @default.
• W2281252973 startingPage "337" @default.
• W2281252973 abstract "Detrital zircon from unconsolidated, Cenozoic sediments from eastern South Africa has been analysed for U–Pb and Lu–Hf isotopes by laser ablation inductively coupled plasma mass spectrometry. Identifiable bedrock sources have made local contributions to the detrital zircon populations, but the dominant zircon components are of regional distribution: late Mesoproterozoic (e Hf  = –5 to +10), Neoproterozoic to early Palaeozoic (e Hf  = –10 to +10), and minor late Palaeozoic (e Hf  ≈ 0). Archaean zircons are scarce even in sediments deposited on exposed Archaean basement or by rivers eroding it. The dominant components cannot be tied to specific first-generation sources in southern Africa or its former Gondwana neighbours. Instead, we see the effect of mixing and remobilization of debris from large parts of the supercontinent in the early Phanerozoic, which was stored in the Karoo basin and other continental cover sequences and shed from there to the present site of deposition. Therefore, data from detrital zircon in these deposits tell us less about the path of detritus from source to sink in a recent sedimentary system than about processes in much earlier erosion–transport–deposition cycles. To facilitate comparison of detrital zircon age distribution patterns, a simple and intuitive method that takes sampling uncertainty explicitly into account is proposed. Supplementary materials: U–Pb and Lu–Hf data, and concordia diagrams and discussion of effects of discordance are available at http://www.geolsoc.org.uk/SUP18884." @default.
• W2281252973 created "2016-06-24" @default.
• W2281252973 creator A5033913456 @default.
• W2281252973 creator A5042413072 @default.
• W2281252973 creator A5076630029 @default.
• W2281252973 date "2015-10-27" @default.
• W2281252973 modified "2023-10-14" @default.
• W2281252973 title "U–Pb and Lu–Hf zircon data in young sediments reflect sedimentary recycling in eastern South Africa" @default.
• W2281252973 cites W1864475283 @default.
• W2281252973 cites W1963713730 @default.
• W2281252973 cites W1965108393 @default.
• W2281252973 cites W1989312311 @default.
• W2281252973 cites W1989332107 @default.
• W2281252973 cites W1991981435 @default.
• W2281252973 cites W1996451493 @default.
• W2281252973 cites W1996562355 @default.
• W2281252973 cites W2001694367 @default.
• W2281252973 cites W2003017642 @default.
• W2281252973 cites W2005416144 @default.
• W2281252973 cites W2006613948 @default.
• W2281252973 cites W2006703366 @default.
• W2281252973 cites W2008064450 @default.
• W2281252973 cites W2010919640 @default.
• W2281252973 cites W2014515321 @default.
• W2281252973 cites W2014934612 @default.
• W2281252973 cites W2019851644 @default.
• W2281252973 cites W2020771786 @default.
• W2281252973 cites W2021954729 @default.
• W2281252973 cites W2023509626 @default.
• W2281252973 cites W2026255147 @default.
• W2281252973 cites W2026968757 @default.
• W2281252973 cites W2034130965 @default.
• W2281252973 cites W2034472228 @default.
• W2281252973 cites W2035631448 @default.
• W2281252973 cites W2038455252 @default.
• W2281252973 cites W2039570402 @default.
• W2281252973 cites W2039872199 @default.
• W2281252973 cites W2040228179 @default.
• W2281252973 cites W2044175358 @default.
• W2281252973 cites W2046991191 @default.
• W2281252973 cites W2048230691 @default.
• W2281252973 cites W2052448030 @default.
• W2281252973 cites W2059723616 @default.
• W2281252973 cites W2060102124 @default.
• W2281252973 cites W2065792360 @default.
• W2281252973 cites W2070836124 @default.
• W2281252973 cites W2071673134 @default.
• W2281252973 cites W2074735230 @default.
• W2281252973 cites W2075740329 @default.
• W2281252973 cites W2080465168 @default.
• W2281252973 cites W2080835780 @default.
• W2281252973 cites W2082066614 @default.
• W2281252973 cites W2084367124 @default.
• W2281252973 cites W2085274161 @default.
• W2281252973 cites W2086675413 @default.
• W2281252973 cites W2087734262 @default.
• W2281252973 cites W2094941598 @default.
• W2281252973 cites W2095535473 @default.
• W2281252973 cites W2098013767 @default.
• W2281252973 cites W2099067742 @default.
• W2281252973 cites W2105119747 @default.
• W2281252973 cites W2117942534 @default.
• W2281252973 cites W2127086666 @default.
• W2281252973 cites W2129866727 @default.
• W2281252973 cites W2138845249 @default.
• W2281252973 cites W2139096563 @default.
• W2281252973 cites W2140357126 @default.
• W2281252973 cites W2152294755 @default.
• W2281252973 cites W2163661859 @default.
• W2281252973 cites W2165007808 @default.
• W2281252973 cites W2165924884 @default.
• W2281252973 cites W2171665987 @default.
• W2281252973 cites W2174216460 @default.
• W2281252973 cites W2267922192 @default.
• W2281252973 cites W2315275671 @default.
• W2281252973 cites W2318795195 @default.
• W2281252973 cites W288477143 @default.
• W2281252973 cites W4249301907 @default.
• W2281252973 doi "https://doi.org/10.1144/jgs2015-006" @default.
• W2281252973 hasPublicationYear "2015" @default.
• W2281252973 type Work @default.
• W2281252973 sameAs 2281252973 @default.
• W2281252973 citedByCount "38" @default.
• W2281252973 countsByYear W22812529732016 @default.
• W2281252973 countsByYear W22812529732017 @default.
• W2281252973 countsByYear W22812529732018 @default.
• W2281252973 countsByYear W22812529732019 @default.
• W2281252973 countsByYear W22812529732020 @default.
• W2281252973 countsByYear W22812529732021 @default.
• W2281252973 countsByYear W22812529732022 @default.
• W2281252973 countsByYear W22812529732023 @default.
• W2281252973 crossrefType "journal-article" @default.
• W2281252973 hasAuthorship W2281252973A5033913456 @default.
• W2281252973 hasAuthorship W2281252973A5042413072 @default.
• W2281252973 hasAuthorship W2281252973A5076630029 @default.
• W2281252973 hasConcept C127313418 @default.
• W2281252973 hasConcept C138170599 @default.
• W2281252973 hasConcept C17409809 @default.

• next