Abstract The McArthur Basin is part of a Proterozoic basin system on the North Australian
Craton that represents a world-class Zn-Pb province. Ore bodies are typically stratiform and …

Abstract The late Paleoproterozoic upper McArthur Group (River Supersequence) is a
dominantly shallow marine carbonate platform sequence. Deeper water shaley rocks of the …

Abstract The southern McArthur Basin is highly prospective for sediment-hosted Zn-Pb-Ag
mineralisation, and hosts the McArthur River and Teena deposits within the Batten Fault …

Palaeoproterozoic sedimentary rocks of the McArthur–Mt Isa–Cloncurry mineral belt of
northern Australia host the world's most important zinc repository, several worldclass Cu and …

Abstract The greater McArthur Basin is an informal term for a Palaeo-to-Mesoproterozoic
sedimentary system that consists of terranes from the McArthur Basin, Birrindudu Basin, and …

Abstract The Paleoproterozoic McArthur Basin (McArthur Group) of northern Australia hosts
world-class sedimentary 'exhalative'(SEDEX) McArthur type Zn–Pb deposits, which are …

Northern Australia contains extensive Proterozoic sedimentary basins that contain organic-
rich rocks with the potential to host both major petroleum accumulations and basin-hosted …

Abstract The Beetaloo Sub‐basin, northern Australia, is considered the main depocentre of
the 1,000‐km scale Mesoproterozoic Wilton package of the greater McArthur Basin–the host …

Abstract The 300-Mt Broken Hill Pb-Zn-Ag orebody is in the Broken Hill Domain, which,
together with the contiguous Olary Domain, constitutes the southern part of the Curnamona …

Mature, rich, potential source beds and adjacent potential reservoir beds exist in the Middle
Proterozoic sequence (1400-1800 Ma) of the McArthur Basin. The McArthur and Nathan …