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Mount Misery. Progress reports and final report to licence expiry/full surrender, for the period 30/11/1981 to 29/11/1985.
Stratabound, chemically precipitated Telfer - type replacement style vein gold was the target of exploration undertaken over an area 25 km north-west of Yunta, which contains good exposures of Neoproterozoic Umberatana Group clastic metasediments that...-
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Copperlinka. Progress and annual reports plus final report to licence expiry/full surrender, for the period 16/4/1991 to 6/6/1997.
Exploration for possible large, potentially open cut - mineable disseminated quartz vein - type syngenetic gold and base metal deposits within a licence area located near Outalpa, 150 km south-west of Broken Hill, has comprised geological mapping,...-
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RB 84/00028 Petrography of 25 specimens from Mount Grainger Goldfield.
Specimens from the Mt Grainger Goldfield include quartzites, sandstones in which kaolinite is believed to represent earlier feldspar, siltstones, shales, diamictites of probable glaciogene origin, granitoids and andesites. Low to moderate temperature...-
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Published: 01 May 1984
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Eurelia - Carrieton area. Progress reports to licence expiry/renewal for the period 27/5/1974 to 26/5/1976.
Continuing exploration for economic stratiform copper occurrences in the Carrieton area has involved considerable further drilling (69 rotary drag bit holes for a total of 2864 m, 19 percussion / precollar cased holes for a total of 2381 m, and 6...-
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Oulnina Park. Progress reports to licence expiry/full surrender, for the period 5/1/1990 to 14/6/1993.
Auriferous quartz/haematite/manganese oxide veins within fine-grained Upper Proterozoic metasedimentary rocks in the Benda Range area, 15 km south-southeast of Mannahill, were investigated by regional surface rock chip geochemical sampling, costeaning...-
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Paratoo. Progress reports to licence expiry/renewal, for the period 1/9/1965 to 31/8/1966.
Examination of potentially economic stratiform copper mineralisation recorded in the Paratoo area, located approximately 60 km north-east of Peterborough, has found that it occurs within Adelaidean shales and siltstones over the apical hinge zone of a...-
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