Middle and Late Ordovician magmatic evolution of the Macquarie Arc, Lachlan Orogen, New South Wales

2007 ◽  
Vol 54 (2-3) ◽  
pp. 181-214 ◽  
Author(s):  
A. J. Crawford ◽  
S. Meffre ◽  
R. J. Squire ◽  
L. M. Barron ◽  
T. J. Falloon
2021 ◽  
Author(s):  
S. Bodorkos ◽  
M.A.S Eastlake ◽  
K. Waltenberg ◽  
K.F. Bull ◽  
P.J. Gilmore ◽  
...  

1986 ◽  
Vol 60 (1) ◽  
pp. 145-157 ◽  
Author(s):  
B. D. Webby ◽  
W. M. Blom

Late Ordovician radiolarians are described from allochthonous limestone breccia deposits of the graptolitic Malongulli Formation of central New South Wales. Included among the forms are the new ‘palaeoactinommid’ genus Kalimnasphaera with new species K. maculosa, the new entactiniid species, Entactinia subulata, and the new anakrusid species, Auliela taplowensis. A number of other entactiniids and the first recorded Ordovician ‘rotasphaerids’ are placed in open nomenclature. Graptolite faunas of the Malongulli Formation indicate that the deposits range in age from the Eastonian Zone of Dicranograptus hians kirki to the Bolindian Zone of Climacograptus uncinatus, that is, from latest Caradoc to early or middle Ashgill in age. This is only the second known well-preserved radiolarian assemblage to be illustrated from Late Ordovician (late Caradoc–Ashgill) successions, and the earliest known from Australia. The radiolarians typically occur in tabularly shaped, laminated lime-mudstone clasts with an abundance of siliceous sponge remains. These clasts appear to be formed from peri-platform ooze of the ‘deeper-water’ slope facies, which became incorporated in debris flows moving into the adjoining basin.


1985 ◽  
Vol 9 (2) ◽  
pp. 143-157 ◽  
Author(s):  
Bryan Stait ◽  
Barry D. Webby ◽  
Ian G. Percival

2013 ◽  
Vol 60 (3) ◽  
pp. 371-412 ◽  
Author(s):  
R. A. Glen ◽  
R. J. Korsch ◽  
R. Hegarty ◽  
A. Saeed ◽  
Y. Poudjom Djomani ◽  
...  

2016 ◽  
Vol 90 (3) ◽  
pp. 433-471 ◽  
Author(s):  
David J. Holloway ◽  
Philip D. Lane

AbstractThe trilobite fauna of the middle Silurian (Telychian to possibly earliest Sheinwoodian) Tomcat Creek limestone in the Broken River Province of north Queensland is dominated by the suborder Illaenina, including illaenimorphs (Illaeninae and Bumastinae) and members of the Scutelluidae. Scutelluidae are most diverse, with eight genera, of whichDolabrapex,Iotoryx,Perizostra, andQuintoniaare new.Perizostrais the first scutelluid with a cephalon that may be described as of phacomorph appearance. Illaenimorphs are represented by three genera, includingOpsypharus, which is regarded as a senior synonym ofParacybantyxbut distinct fromFailleanawith which it has been placed in synonymy by some authors. Thirteen species are new:Cybantyx?ergodes,Opsypharus pandanensis,Australoscutellum talenti,Dolabrapex acomus,Illaenoscutellum psephos,Iotoryx clarksoni,Japonoscutellum mawsonae,J. drakton,J. fractum,Kosovopeltis avita,Perizostra campbelli,Quintonia arata, andQ. pavo. A species ofStenopariais placed in open nomenclature. The species ofAustraloscutellum,Illaenoscutellum, and possiblyKosovopeltisare the oldest known representatives of those genera. These genera andJaponoscutellumare also common in faunas from limestones of Wenlock to Ludlow age in central western New South Wales, reflecting the similarity in lithofacies. The monotypic Late Ordovician genusCraigheadia, which has been regarded as a scutelluid, belongs to the Lichidae and is probably a junior synonym ofLeiolichas.


2007 ◽  
Vol 54 (2-3) ◽  
pp. 215-241 ◽  
Author(s):  
R. A. Glen ◽  
R. Spencer ◽  
A. Willmore ◽  
V. David ◽  
R. J. Scott

2007 ◽  
Vol 54 (2-3) ◽  
pp. 137-141 ◽  
Author(s):  
A. J. Crawford ◽  
R. A. Glen ◽  
D. R. Cooke ◽  
I. G. Percival

1985 ◽  
Vol 49 (353) ◽  
pp. 591-599 ◽  
Author(s):  
J. W. Pemberton ◽  
R. Offler

SynopisClinopyroxene phenocrysts and groundmass crystals are relict phases in altered basalt and basaltic andesite lavas, and arenites of the Cudgegong Volcanics and Toolamanang Volcanics, Cudgegong-Mudgee district, New South Wales. Petrography, field relationships and clinopyroxene compositions indicate that basaltic blocks in the latter unit are reworked from the Cudgegong Volcanics. Clinopyroxene phenocrysts show a restricted compositional range and minor Feenrichment from core to rim, features considered indicative of a calc-alkaline parent magma. It is proposed that the Cudgegong Volcanics crystallized under hydrous conditions, at least in the later stages, with rising fO2 resulting in a Fe-Ti oxide crystallizing as a primary phase. The clinopyroxenes are considered to have crystallized at moderate (5–6 kbar) and falling pressures and at minimum temperatures in the range 900 to 1000°C. Coupled substitutions affecting the “other” components in the clinopyroxene structural formula indicate that the ivAl-viFe3+, ivAl-viAl and ivAl-viTi4+ couples are important. The Sofala Volcanics, south of the study area, and the Cudgegong Volcanics are similar in age, petrography and stratigraphic position, and contain relict clinopyroxenes which are chemically similar. This suggests that the units are laterally equivalent and adds further evidence to the proposal that an oceanic island arc system was active in central western New South Wales during the Late Ordovician.


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