This paper introduces a formal lithostratigraphic scheme for major subdivisions of the Olary Domain, and compares these subdivisions to those of the Broken Hill Domain, these two domains being the main components of the Curnamona Province. The scheme...

A tenement area located 25 km south-west of Olary was taken up for exploration because in the licensees' opinion it is favourably located on the southern margin of the Curnamona Craton, and covers Willyama Supergroup metasediments and metavolcanics...

This field guidebook provides brief geological summaries to sites in South Australia that were visited during the 2006 Broken Hill Exploration Initiative pre-conference excursion. Figures show the location of the field area and approximate location of...

Four areas on the south-western margin of the Palaeo-Mesoproterozoic Willyama Inliers were mapped in detail to elucidate the nature of their lithostratigraphy, structure and mineralisation. These basement inliers are composed of...

The excursion to the Old Boolcoomata region of the Olary Domain, Curnamona Province, in South Australia presents most of the stratigraphy of the late Palaeoproterozoic Willyama Supergroup and evidence for its complex deformation during the ~1600 Ma...

In May 2004 the Minister for the Department of Environment and Heritage purchased Bimbowrie Station pastoral lease. The station was purchased because it encompasses part of the Olary Ranges, which is part of the environmentally important Broken Hill...

The aim of this report is to provide a summary of the present status of the geology of the Olary Domain, Curnamona Province. It gives a comprehensive, referenced description of all known interpretations of Willyama Supergroup basement stratigraphy,...

Approximately 30 square km of outcrop of Palaeoproterozoic basement rocks in the vicinity of Ameroo Hill were geologically mapped by the author at 1:10,000 scale, with the aim of identifying meso- and macroscopic rock structures and lithologically...

The Curnamona Province is the southern remnant of the Palaeoproterozoic Pb-Zn belt, and represents but a small fragment of the original superbasin. Geological data supports the idea of the basin being a rift, with sediments in the Broken Hill Domain...

Geochemical and isotopic data from mantle-derived mafic rocks provide important constraints on our understanding of the composition and evolution of the lithosphere through time. Since the lithosphere is sensitive to tectonic processes such as...