FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2082210367> ?p ?o ?g. }

• W2082210367 endingPage "220" @default.
• W2082210367 startingPage "201" @default.
• W2082210367 abstract "Abstract SHRIMP U–Pb analyses are reported for a detrital zircon population from a sample of sillimanite-bearing quartzite from the Narryer sedimentary succession in the Narryer Terrane of the northwestern Yilgarn Craton. The detrital zircons define two distinctive age groups, an older group from 4000 Ga to 4280 Ma and a younger group from 3750 to 3250 Ma. The abundance of older group zircons of about 12% far exceeds the abundance of about 2% reported in the first discovery of ancient zircons in a quartzite from the Narryer metasediments, and is equivalent to the abundance of >3900 Ma zircons in metaconglomerate sample W74 from the Jack Hills, confirmed by new measurements reported in this paper. Most analyses of the Narryer and the Jack Hills detrital zircon populations are discordant. The Jack Hills zircon analyses are dominated by strong recent Pb loss whereas the Narryer zircon analyses have had a more complex history and have experienced at least one Pb loss event, possibly associated with the high-grade metamorphism at ca. 2700 Ma, and a further disturbance of the U–Pb systems during relatively recent times. Although the number of analyses is limited and many of the zircon analyses are discordant, the age distributions of the older (>3900 Ma) zircons from the Narryer and Jack Hills samples are different, suggesting a complex provenance for the ancient zircons. The distribution of ages in the younger population of Mt Narryer zircons is similar to that reported for zircons from the surrounding Meeberrie gneiss, supporting previous suggestions that zircons from the gneisses or their precursors were a major contributor to the detrital zircon suite. The younger zircon population from Jack Hills sample (W74), lacks the strong age peak from 3600 to 3750 Ma present in the Narryer zircon population, and conversely the strong zircon age group at ca. 3350–3500 Ma in the Jack Hills population is only weakly represented in the Narryer zircon population. The age distributions for the Narryer and the Jack Hills zircon populations are taken as benchmarks for comparing zircon populations from quartzite occurrences elsewhere in the Yilgarn Craton." @default.
• W2082210367 created "2016-06-24" @default.
• W2082210367 creator A5032492885 @default.
• W2082210367 creator A5050298271 @default.
• W2082210367 date "2006-11-01" @default.
• W2082210367 modified "2023-09-24" @default.
• W2082210367 title "High abundance of early Archaean grains and the age distribution of detrital zircons in a sillimanite-bearing quartzite from Mt Narryer, Western Australia" @default.
• W2082210367 cites W1615737483 @default.
• W2082210367 cites W1963698123 @default.
• W2082210367 cites W1965597921 @default.
• W2082210367 cites W1965954654 @default.
• W2082210367 cites W1972544114 @default.
• W2082210367 cites W1980343879 @default.
• W2082210367 cites W1988503846 @default.
• W2082210367 cites W1989194022 @default.
• W2082210367 cites W1989286012 @default.
• W2082210367 cites W1989982832 @default.
• W2082210367 cites W1992585057 @default.
• W2082210367 cites W1996920988 @default.
• W2082210367 cites W1997040345 @default.
• W2082210367 cites W1997227702 @default.
• W2082210367 cites W2006991140 @default.
• W2082210367 cites W2009215943 @default.
• W2082210367 cites W2010781943 @default.
• W2082210367 cites W2012118212 @default.
• W2082210367 cites W2013451364 @default.
• W2082210367 cites W2017075044 @default.
• W2082210367 cites W2022714824 @default.
• W2082210367 cites W2028759147 @default.
• W2082210367 cites W2032917647 @default.
• W2082210367 cites W2038542022 @default.
• W2082210367 cites W2040715870 @default.
• W2082210367 cites W2057208829 @default.
• W2082210367 cites W2057709663 @default.
• W2082210367 cites W2059723616 @default.
• W2082210367 cites W2062771554 @default.
• W2082210367 cites W2063745658 @default.
• W2082210367 cites W2064861118 @default.
• W2082210367 cites W2080795567 @default.
• W2082210367 cites W2086642743 @default.
• W2082210367 cites W2088454958 @default.
• W2082210367 cites W2089423835 @default.
• W2082210367 cites W2144457675 @default.
• W2082210367 cites W2145604970 @default.
• W2082210367 cites W2147199686 @default.
• W2082210367 cites W2152292599 @default.
• W2082210367 cites W4243660572 @default.
• W2082210367 doi "https://doi.org/10.1016/j.precamres.2006.07.008" @default.
• W2082210367 hasPublicationYear "2006" @default.
• W2082210367 type Work @default.
• W2082210367 sameAs 2082210367 @default.
• W2082210367 citedByCount "35" @default.
• W2082210367 countsByYear W20822103672012 @default.
• W2082210367 countsByYear W20822103672013 @default.
• W2082210367 countsByYear W20822103672014 @default.
• W2082210367 countsByYear W20822103672017 @default.
• W2082210367 countsByYear W20822103672018 @default.
• W2082210367 countsByYear W20822103672019 @default.
• W2082210367 countsByYear W20822103672020 @default.
• W2082210367 countsByYear W20822103672021 @default.
• W2082210367 crossrefType "journal-article" @default.
• W2082210367 hasAuthorship W2082210367A5032492885 @default.
• W2082210367 hasAuthorship W2082210367A5050298271 @default.
• W2082210367 hasConcept C127313418 @default.
• W2082210367 hasConcept C149347711 @default.
• W2082210367 hasConcept C151730666 @default.
• W2082210367 hasConcept C173776410 @default.
• W2082210367 hasConcept C17409809 @default.
• W2082210367 hasConcept C199978012 @default.
• W2082210367 hasConcept C202539814 @default.
• W2082210367 hasConcept C205649164 @default.
• W2082210367 hasConcept C2777229588 @default.
• W2082210367 hasConcept C2778849375 @default.
• W2082210367 hasConcept C2779870107 @default.
• W2082210367 hasConcept C2780733770 @default.
• W2082210367 hasConcept C505870484 @default.
• W2082210367 hasConcept C58640448 @default.
• W2082210367 hasConcept C77077793 @default.
• W2082210367 hasConcept C86803240 @default.
• W2082210367 hasConceptScore W2082210367C127313418 @default.
• W2082210367 hasConceptScore W2082210367C149347711 @default.
• W2082210367 hasConceptScore W2082210367C151730666 @default.
• W2082210367 hasConceptScore W2082210367C173776410 @default.
• W2082210367 hasConceptScore W2082210367C17409809 @default.
• W2082210367 hasConceptScore W2082210367C199978012 @default.
• W2082210367 hasConceptScore W2082210367C202539814 @default.
• W2082210367 hasConceptScore W2082210367C205649164 @default.
• W2082210367 hasConceptScore W2082210367C2777229588 @default.
• W2082210367 hasConceptScore W2082210367C2778849375 @default.
• W2082210367 hasConceptScore W2082210367C2779870107 @default.
• W2082210367 hasConceptScore W2082210367C2780733770 @default.
• W2082210367 hasConceptScore W2082210367C505870484 @default.
• W2082210367 hasConceptScore W2082210367C58640448 @default.
• W2082210367 hasConceptScore W2082210367C77077793 @default.
• W2082210367 hasConceptScore W2082210367C86803240 @default.
• W2082210367 hasIssue "3-4" @default.
• W2082210367 hasLocation W20822103671 @default.
• W2082210367 hasOpenAccess W2082210367 @default.

• next