Geological Society of America

T174 Precambrian Basin Analysis

Thursday, 29 October 2020
10:00 AM - 12:00 PM
Meeting Rooms

DETRITAL ZIRCON PROVENANCE RECORD OF BASIN TECTONIC GEOGRAPHY: IMPLICATIONS FROM THE MESOPROTEROZOIC WILTON PACKAGE, GREATER MCARTHUR BASIN, NORTHERN AUSTRALIA

Paper number: T174-11
Program: Technical Sessions
Time: 10:50 AM – 10:55 AM

Authors

Bo Yang Presenting Author
Adelaide, SA
Alan S. Collins
Tectonics and Earth Systems (TES) Group and Mineral Exploration CRC, Adelaide, SA
Morgan L. Blades
Tectonics and Earth Systems (TES) Group and Mineral Exploration CRC, Adelaide, SA
Tim J. Munson
Department of Primary Industry and Resources, Darwin, NT
Justin Payne
University of South Australia, Adelaide SA, SA
Stijn Glorie
The University of Adelaide, Adelaide, SA
Juraj Farkas
Metal Isotope Group (MIG), Adelaide, SA

Abstract

The ca. 1.5–1.3 Ga Wilton package, the upper succession of the greater McArthur Basin, preserves detailed tectono-sedimentary evidence for the Mesoproterozoic evolution of the North Australia Craton (NAC). In addition, it is an valuable global sedimentary repository for the poorly explored Mesoproterozoic. New detrital zircon U–Pb age and Lu–Hf isotope data, collected from multiple, geographically separated, basins that make up the Wilton package, are compiled with previously published data to illuminate the basin evolution. The spatial and temporal variation in sedimentary provenance illustrates two major geographic changes that correspond to continent-scale tectonic convulsions of the NAC during the Mesoproterozoic. The first is shown by the influx of sediment sourced from east and southeast terranes. This has been linked to the rifting between the Proterozoic Australia and the Laurentia at about 1.45 Ga, resulting the uplift of the eastern margin of the NAC-SAC (South Australia Craton). The second basin geographic change is illustrated by a ca. 1.32 Ga flux of southerly-sourced detritus that is interpreted to be tectonically driven by the uplift of the southern NAC, during the subduction/closure of the Mirning Ocean.

Spatially, sediment in the Wilton package is separated into two deposition systems―sedimentary rocks within the Birrindudu Basin, the western component of the Wilton package, have different detrital signatures to other Wilton package successions found east of the Daly Waters Fault Zone, in the Beetaloo Sub-basin, the McArthur Basin and the South Nicholson Basin. The Daly Waters Fault Zone is interpreted as an ancient bathymetric high, blocking sediment transport. Although they differ in sources, both the Birrindudu basin and the eastern Wilton package record coeval shifts of basin provenance to southern sources. The coherent evolution of basin provenance indicates a consistent tectono-sedimentation history, and links the Birrindudu Basin and the other Wilton successions in a tectonic framework.

Geological Society of America Abstracts with Programs. Vol. 52, No. 6

doi: 10.1130/abs/2020AM-356703

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