FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2000329036> ?p ?o ?g. }

• W2000329036 endingPage "500" @default.
• W2000329036 startingPage "475" @default.
• W2000329036 abstract "Provenance data from Paleoproterozoic and possible Archean sedimentary units in the central eastern Gawler Craton in southern Australia form part of a growing dataset suggesting that the Gawler Craton shares important basin formation and tectonic time lines with the adjacent Curnamona Province and the Isan Inlier in northern Australia. U–Pb dating of detrital zircons from the Eba Formation, previously mapped as the Paleoproterozoic Tarcoola Formation, yields exclusively Archean ages (ca 3300–2530 Ma), which are consistent with evolved whole-rock Nd and zircon Hf isotopic data. The absence of Paleoproterozoic detrital grains in a number of sequences (including the Eba Formation), despite the proximity of voluminous Paleoproterozoic rock units, suggests that the Eba Formation may be part of a Neoarchean or early Paleoproterozoic cover sequence derived from erosion of a multi-aged Archean source region. The ca 1715 Ma Labyrinth Formation, unconformably overlying the Eba Formation, shares similar depositional timing with other basin systems in the Gawler Craton and the adjacent Curnamona Province. Detrital zircon ages in the Labyrinth Formation range from Neoarchean to Paleoproterozoic, and are consistent with derivation from >1715 Ma components of the Gawler Craton. Zircon Hf and whole-rock Nd isotopic data also suggest a source region with a mixed crustal evolution (εNd –6 to –4.5), consistent with what is known about the Gawler Craton. Compared with the lower Willyama Supergroup in the adjacent Curnamona Province, the Labyrinth Formation has a source more obviously reconcilable with the Gawler Craton. Stratigraphically overlying the Eba and Labyrinth Formations is the 1656 Ma Tarcoola Formation. Zircon Hf and whole-rock Nd isotopic data indicate that the Tarcoola Formation was sourced from comparatively juvenile rocks (εNd –4.1 to + 0.5). The timing of Tarcoola Formation deposition is similar to the juvenile upper Willyama Supergroup, further strengthening the stratigraphic links between the Gawler and Curnamona domains. Additionally, the Tarcoola Formation is similar in age to extensive units in the Mt Isa and Georgetown regions in northern Australia, also shown to be isotopically juvenile. These juvenile sedimentary rocks contrast with the evolved underlying sequences and hint at the existence of a large-scale ca 1650 Ma juvenile basin system in eastern Proterozoic Australia." @default.
• W2000329036 created "2016-06-24" @default.
• W2000329036 creator A5017564164 @default.
• W2000329036 creator A5026908916 @default.
• W2000329036 creator A5032161414 @default.
• W2000329036 creator A5056695911 @default.
• W2000329036 date "2011-07-01" @default.
• W2000329036 modified "2023-09-23" @default.
• W2000329036 title "Provenance of late Paleoproterozoic cover sequences in the central Gawler Craton: exploring stratigraphic correlations in eastern Proterozoic Australia using detrital zircon ages, Hf and Nd isotopic data" @default.
• W2000329036 cites W1012135854 @default.
• W2000329036 cites W1514394155 @default.
• W2000329036 cites W1968438005 @default.
• W2000329036 cites W1977911355 @default.
• W2000329036 cites W1979636222 @default.
• W2000329036 cites W1980531461 @default.
• W2000329036 cites W1983367474 @default.
• W2000329036 cites W1985026590 @default.
• W2000329036 cites W1985620741 @default.
• W2000329036 cites W1989982832 @default.
• W2000329036 cites W1990277683 @default.
• W2000329036 cites W1994916635 @default.
• W2000329036 cites W1996055672 @default.
• W2000329036 cites W1996920988 @default.
• W2000329036 cites W1998081253 @default.
• W2000329036 cites W2006916087 @default.
• W2000329036 cites W2008650987 @default.
• W2000329036 cites W2015876559 @default.
• W2000329036 cites W2018695532 @default.
• W2000329036 cites W2020779706 @default.
• W2000329036 cites W2020973699 @default.
• W2000329036 cites W2022391288 @default.
• W2000329036 cites W2023179220 @default.
• W2000329036 cites W2038813050 @default.
• W2000329036 cites W2045889087 @default.
• W2000329036 cites W2048230691 @default.
• W2000329036 cites W2049734018 @default.
• W2000329036 cites W2049825905 @default.
• W2000329036 cites W2051273227 @default.
• W2000329036 cites W2051750046 @default.
• W2000329036 cites W2055242142 @default.
• W2000329036 cites W2060461428 @default.
• W2000329036 cites W2080325016 @default.
• W2000329036 cites W2086770043 @default.
• W2000329036 cites W2090206242 @default.
• W2000329036 cites W2090620804 @default.
• W2000329036 cites W2098707777 @default.
• W2000329036 cites W2100564045 @default.
• W2000329036 cites W2111858108 @default.
• W2000329036 cites W2122562985 @default.
• W2000329036 cites W2133650428 @default.
• W2000329036 cites W2134337167 @default.
• W2000329036 cites W2141472067 @default.
• W2000329036 cites W2160670349 @default.
• W2000329036 cites W2169766597 @default.
• W2000329036 cites W2346816322 @default.
• W2000329036 cites W4244634768 @default.
• W2000329036 cites W4245087046 @default.
• W2000329036 cites W4252228515 @default.
• W2000329036 cites W4367337346 @default.
• W2000329036 cites W2069794648 @default.
• W2000329036 doi "https://doi.org/10.1080/08120099.2011.577753" @default.
• W2000329036 hasPublicationYear "2011" @default.
• W2000329036 type Work @default.
• W2000329036 sameAs 2000329036 @default.
• W2000329036 citedByCount "21" @default.
• W2000329036 countsByYear W20003290362013 @default.
• W2000329036 countsByYear W20003290362014 @default.
• W2000329036 countsByYear W20003290362015 @default.
• W2000329036 countsByYear W20003290362016 @default.
• W2000329036 countsByYear W20003290362017 @default.
• W2000329036 countsByYear W20003290362018 @default.
• W2000329036 countsByYear W20003290362019 @default.
• W2000329036 countsByYear W20003290362020 @default.
• W2000329036 countsByYear W20003290362022 @default.
• W2000329036 countsByYear W20003290362023 @default.
• W2000329036 crossrefType "journal-article" @default.
• W2000329036 hasAuthorship W2000329036A5017564164 @default.
• W2000329036 hasAuthorship W2000329036A5026908916 @default.
• W2000329036 hasAuthorship W2000329036A5032161414 @default.
• W2000329036 hasAuthorship W2000329036A5056695911 @default.
• W2000329036 hasConcept C127313418 @default.
• W2000329036 hasConcept C147717901 @default.
• W2000329036 hasConcept C149347711 @default.
• W2000329036 hasConcept C151730666 @default.
• W2000329036 hasConcept C17409809 @default.
• W2000329036 hasConcept C202746551 @default.
• W2000329036 hasConcept C2778849375 @default.
• W2000329036 hasConcept C2780049196 @default.
• W2000329036 hasConcept C77928131 @default.
• W2000329036 hasConcept C93033518 @default.
• W2000329036 hasConceptScore W2000329036C127313418 @default.
• W2000329036 hasConceptScore W2000329036C147717901 @default.
• W2000329036 hasConceptScore W2000329036C149347711 @default.
• W2000329036 hasConceptScore W2000329036C151730666 @default.
• W2000329036 hasConceptScore W2000329036C17409809 @default.
• W2000329036 hasConceptScore W2000329036C202746551 @default.
• W2000329036 hasConceptScore W2000329036C2778849375 @default.
• W2000329036 hasConceptScore W2000329036C2780049196 @default.

• next