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Autor:
Anna Maria Fioretti, Clive R. Calver, Lance P. Black, John L. Everard, M.P. McClenaghan, Chris Foudoulis, A Brown, R. J. Korsch
Publikováno v:
Australian journal of earth sciences 57 (2010): 933–968. doi:10.1080/08120099.2010.509407
info:cnr-pdr/source/autori:Black L.; Everard J.; McClenaghan M.; Korsch R.; Calver C.; Fioretti A.; Brown A.; Foudoulis C./titolo:Controls on Devonian-Carboniferous magmatism in Tasmania, based on inherited zircon age patterns, Sr, Nd and Pb isotopes, and major and trace element geochemistry./doi:10.1080%2F08120099.2010.509407/rivista:Australian journal of earth sciences/anno:2010/pagina_da:933/pagina_a:968/intervallo_pagine:933–968/volume:57
info:cnr-pdr/source/autori:Black L.; Everard J.; McClenaghan M.; Korsch R.; Calver C.; Fioretti A.; Brown A.; Foudoulis C./titolo:Controls on Devonian-Carboniferous magmatism in Tasmania, based on inherited zircon age patterns, Sr, Nd and Pb isotopes, and major and trace element geochemistry./doi:10.1080%2F08120099.2010.509407/rivista:Australian journal of earth sciences/anno:2010/pagina_da:933/pagina_a:968/intervallo_pagine:933–968/volume:57
Devonian-Carboniferous granites are widespread in Tasmania. In eastern Tasmania, Devonian granites intrude Ordovician-Early Devonian quartz-rich turbidites of the Mathinna Supergroup. The earliest (*400 Ma) I-type granodiorites may be arc-related. Fo
Autor:
Geoff Fraser, David A. Foster, William L. Griffin, Christopher J. Adams, R. J. Korsch, C. G. Murray, Lance P. Black, Chris Foudoulis
Publikováno v:
Australian Journal of Earth Sciences. 56:655-685
In easternmost Australia, the New England Orogen contains a geological record dominated by subduction-related rocks, with plate convergence during the Late Devonian to Triassic being related to a west-dipping subduction system, assuming present-day o
Publikováno v:
Australian Journal of Earth Sciences. 56:S125-S137
Detrital zircons from the Eocene Garford paleovalley, central South Australia, were derived from two main sources: (i) local Archean–Mesoproterozoic rocks of the Gawler Craton exposed in the paleocatchment, including the 2525–2440 Ma Mulgathing C
Publikováno v:
ResearcherID
Hydrothermal zircons occur as an integral component of the alteration and mineralization assemblage in the Gidginbung high sulphidation Au-Ag-(Cu) deposit in the Lachlan Fold Belt, Australia. Their hydrothermal origin is demonstrated by (1) their par
Publikováno v:
Australian Journal of Earth Sciences. 52:807-829
A series of new Sensitive High-Resolution Ion MicroProbe (SHRIMP) U – Pb ages is presented for Palaeozoic (mainly Devonian and Carboniferous) granites from Tasmania. In virtually all instances the new ages are significantly older than previously de
Autor:
Lance P. Black
Publikováno v:
Geostandards and Geoanalytical Research. 29:169-182
Data from a series of extended analytical sessions using a range of different zircon reference samples have been used to investigate the periodic derivation of abnormal 207Pb/206Pb ages during microbeam analysis%For the Canberra SHRIMP II, this pheno
Publikováno v:
Australian Journal of Earth Sciences. 52:385-401
The Einasleigh Metamorphics form part of the Etheridge Group and are interpreted as the lowest exposed part of the Georgetown Inlier of north Queensland. Due to a dearth of interbedded felsic igneous rocks that would be suitable for isotopic dating,
Publikováno v:
Australian Journal of Earth Sciences. 52:1-25
In the western part of the Mt Isa Inlier one of the most obvious lithostratigraphic correlations is the Torpedo Creek Quartzite (Lawn Hill Platform) and the Warrina Park Quartzite (Leichhardt River Fault Trough). These two sand bodies form the basal
Publikováno v:
Australian Journal of Earth Sciences. 51:885-900
Detrital zircons from 13 Late Mesoproterozoic to Early Neoproterozoic sandstones and two Palaeozoic sandstones from Tasmania were dated in order to improve constraints on depositional ages, to test correlation between Proterozoic inliers, and to char