URL: https://geoscience.data.qld.gov.au/dataset/cr123408 The project area lies within the Western Succession of the Mount Isa to McArthur River Block mineralised sequence. Mt Isa/McArthur Basin mineralised sequence is one of the world’s major copper, lead, zinc and silver provinces hosting several deposits including the Mt Isa, George‐Fisher, Hilton, Gunpowder, Century, Valhalla (U), Westmoreland (U), Constance Range (Fe) deposits. The Western Succession copper‐zinc‐lead‐silver deposits make the region one of Australia’s most sought‐after target regions. The currently operating mines to the north and south of the project areas along the same structures confirms this part of the region’s potential to host large deposits. Within the Mt Isa Block, four Proterozoic tectono‐stratigraphic terrains are recognized which comprise an older basement core overlain by three younger Proterozoic sedimentary sequences referred to as Cover Sequences 1, 2 and 3. These cover sequences are related to major episodes of intra‐cratonic rift and sag phase sedimentation. The Middle Proterozoic rocks record a complex history of intra‐continental rifting and subsidence during the period 1,800 to 1,590 million years (Ma), followed by compression, basin inversion and regional wrenching during the Isan Orogeny (1,590 to 1,500 Ma). Within the Western Succession, Cover Sequence 3 east of the Mount Gordon Fault is assigned to the Mt Isa Group (maximum thickness of 4,500 m) within the Leichhardt River Fault Trough. The equivalent sequence to the west of the fault is assigned to the McNamara Group (maximum thickness of 8,500 m) deposited in the Lawn Hill Platform. In the far north of the Mt Isa Block, this rock sequence is termed the Fickling Group. Cover Sequence 3 hosts many of the significant base metal deposits within the Mount Isa Block, including the Mt Isa, Mount Gordon, Mount Oxide, Hilton and George Fisher base metal deposits within the Mt Isa Group, and the Lady Loretta, Century and Lady Annie deposits within the similar‐aged McNamara Group.

URL: https://geoscience.data.qld.gov.au/dataset/cr081442 EPM 15896, SUNDAY CREEK IRON AND OTHER MINERALS PROJECT, ANNUAL REPORT FOR PERIOD ENDING 16/11/2013

URL: https://geoscience.data.qld.gov.au/dataset/cr089038 EPM 15896, SUNDAY CREEK IRON AND OTHER MINERALS PROJECT, ANNUAL REPORT FOR PERIOD ENDING 16/11/2014

URL: https://geoscience.data.qld.gov.au/dataset/cr021558 EPM 4729, COPPERMINE CREEK, FINAL REPORT FOR PERIOD ENDING 18/1/1990

URL: https://geoscience.data.qld.gov.au/dataset/cr104209 EPM 15896, SUNDAY CREEK IRON AND OTHER MINERALS PROJECT, ANNUAL REPORT FOR PERIOD ENDING 16/11/2017

URL: https://geoscience.data.qld.gov.au/dataset/cr055325 GSQ PUBLICATION 169 ON SOME MINES AND MINERAL DEPOSITS AT THE HEADS OF THE BRISBANE, BURNETT, AND MARY RIVERS (WITH FIVE PLATES)

URL: https://geoscience.data.qld.gov.au/dataset/cr000304 EPM 39, INSKIP AND FRASER, HEAVY MINERALS INVESTIGATION, INTERIM REPORT FOR PERIOD 1/4/1958 TO 30/6/1958

URL: https://geoscience.data.qld.gov.au/dataset/cr134095 EPM 26180 Mt Aplin project was obtained to explore for a range of different styles of mineralisation. Exploration has focussed on phosphate mineralisation in the along the margins of the Cambrian Georgina Basin and base metal mineralisation within the Proterozoic in areas of the tenement with less than 200 m of Phanerozoic sediments. Desktop studies included a prospectivity assessment for phosphate mineralisation and Proterozoic IOCG exploration targets that could support current operations at Osborne. Previous explorers have completed significant work including modern geophysical surveys, RC drilling and diamond drilling. Numerous targets have been well-tested by these previous explorers with limited success. The EPM is considered to possess low potential for economic phosphate or IOCG mineralisation.

URL: https://geoscience.data.qld.gov.au/dataset/cr019615 EPM 4729, COPPERMINE CREEK, SIX MONTHLY REPORT FOR PERIOD ENDING 31/10/1988

URL: https://geoscience.data.qld.gov.au/dataset/cr055570 GSQ REPORT 85, COPPER MINING IN THE CLONCURRY AND MT ISA FIELDS, 1971