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 ca 1640 Ma Barney Creek Formation is a mostly fine-grained silicicastic unit of
the McArthur Group in the southern McArthur Basin of northern Australia. It is one of the most …

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 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 late Palaeoproterozoic (Statherian) McArthur Group comprises a thick (~ 5
km) sequence of platformal stromatolitic dolostone and clastic sediment with local pyritic …

Rocks of the lower McNamara Group (including the Torpedo Creek, Gunpowder Creek,
Paradise Creek, and Esperanza formations) form part of the extensive late Paleoproterozoic …

The River Supersequence represents a 2nd‐order accommodation cycle of approximately
15 million years duration in the Isa Superbasin. The River Supersequence comprises eight …

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

Abstract The ca. 1730 Ma Wollogorang Formation is a mixed carbonate-siliciclastic unit in
the southern McArthur Basin of northern Australia. It is an exploration target for base metals …

The ages of deposition and metamorphism of low-grade Precambrian metasedimentary
sequences can be difficult to define in the absence of interlayered volcanogenic rocks …