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Abstract

The 1815-1705 Ma Redbank package is a 3-6 km thick succession of shallow marine to braided
fluvial sandstone and lesser conglomerate, mudstone, carbonates and rhyolitic-basaltic volcanics
and high-level intrusions. It forms the base of the Palaeo proterozoic McArthur Basin in northern
Australia.
In the southern McArthur Basin, the Tawallah Group is the best exposed stratigraphic
component of this package. Coarse-grained facies at the base of the Group formed in a
proximal-medial braided fluvial environment and are overlain by widespread sheets of supermature
quartzarenite and intervening flood basalt. These enigmatic sandstone sheets contain features
consistent with deposition in a complex high-energy shallow marine, fluvial and aeolian setting
on an extensive low-gradient shelf Overlying mudstones and carbonates were deposited on a
shallow epeiric shelf and coastal sabkha fringe that onlapped basement tectonic ridges.
A regional sequence boundary formed during subsequent regional uplift and local synsedimentary
deformation, and was followed by deposition of another widespread quartzarenite sheet.
The overlying succession of fine-grained sandstone, mudstone, carbonate and evaporitic
redbeds suggest more diverse depositional settings. Marginal marine salina, near-shore
peritidal, storm-dominated shelf and moderately deep water settings, with periodic restriction
to the marine realm, fluctuating accommodation rates and minor synsedimentary faulting are all
recorded.
Regional-scale dolerite sills and an extensive stacked succession of basalt sheets were emplaced
sequentially as widely-dispersed invasive flows under a thin blanket of wet unconsolidated sediment
and peperite. Volcanism was locally associated with uplift and emplacement of polymict debris
flows and breccia bodies. This was followed by deposition of a complex association of clastic
sediments and felsic volcanics and intrusion of high-level plutons (upper Tawallah Group).
Sheet-like rhyolitic lavas with abrupt talus-lined margins evolved via non-explosive eruption and
long-term viscous flow. This was facilitated by low water content and high and continuous eruption
temperature and effusion rate. Complex ephemeral alluvial and debris flow aprons formed adjacent
to the lavas, recording the generation, erosional denudation and final burial of a dynamic
high-relief volcano-tectonic landscape. Epiclastic materials were reworked in bordering lakes and
low-relief braid plains that prograded radially away from the volcanic centres. Periods between
magmatic events were characterised by deposition of widespread immature sandstone sheets in
extensive high-energy ephemeral to perennial braided fluvial settings and the development of
low-relief regional disconformities. Concurrent pluton emplacement in the northern
McArthur Basin generated a series of structural domes with peripheral deformation.
Accommodation space for intrusion was provided by decollement at ductility transitions, upward
flexuring, outward gravity slide and vertical displacement of overlying sediments. Detailed stratigraphic and facies analysis of the Tawallah Group has enabled the development
of a tectonostratigraphic framework for the entire Redbank package. Four second order
subdivisions are recognised (Yirrumanja, Liverpool, Costello and Mitchell mesopackages)
that facilitate a clearer, integrated regional understanding of the lithology, timing and geographic
distribution of basin phases. The package concept is also applied to the composite McArthur Basin
system as a whole. Five distinct and regionally coherent basin phases are recognised (Redbank,
Goyder, Glyde, Favenc and Wilton packages). These were deposited in a dynamic tectonic
environment over a period of -350 m.y.
Geochemical characterisation of Proterozoic igneous phases in northern Australia has confirmed
many lithostratigraphic correlations in the McArthur Basin. Felsic units show temporal and spatial
variation in geochemistry that reflects partial melting of heterogeneous Archaean mafic lower crust
due to the emplacement oflarge basaltic magma chambers and radiogenic heating. The McArthur
Basin contains five main mafic igneous phases with typical flood basalt attributes, spanning a
period of -480 m.y. Magmas were derived by partial melting of chemically-stratified lower
lithosphere and do not exhibit a plume or rift signature.
A convergent intracratonic setting is proposed for the Redbank package. Basin architecture
reflects diverse subsidence mechanisms operating inboard of the active southern margin of the
North Australian Craton (Strangways arc). Wedge-shaped and magmatic-related basin architectures
formed during subduction. Subsidence was influenced by dynamic topography, thermally- and
mechanically-driven viscoelastic behaviour of heterogeneous crust, magmatic underplating,
lithospheric phase transformations, and local transtension and isostatic loading. Local growthfault
architecture formed by incipient back-arc extension. Magmatism was driven by a persistent
thermal anomaly related to insulative heating and a transient convective roll emanating from the
Strangways arc, that eroded the lower lithosphere and generated a magma pool. Migration of
magma into lower-crustal magma chambers and to the surface took place at transtensional sites
along lithosphere-scale strike-slip faults. Regional unconformities and elongate and wedge basin
architectures formed in the Redbank package during periodic terrane accretion events at the
Strangways arc. Subsidence was influenced largely by transmission of in-plane stress through the
lithosphere to produce lithosphere-scale folding, viscoelastic deflections of the lithosphere, and
transtensional strike-slip and flexural back-bulge basins. Local elongate magmatic grabens are
interpreted as impactogens resulting from indentor tectonics.

Item Type:	Thesis - PhD
Authors/Creators:	Rawlings, D
Additional Information:	Copyright the Author - The University is continuing to endeavour to trace the copyright owner(s) and in the meantime this item has been reproduced here in good faith. We would be pleased to hear from the copyright owner(s).
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