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Cloncurry District

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Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP453.4
EISBN: 9781786203342
... Abstract Iron oxide–Cu–Au (IOCG) deposits encompass a range of ore body shapes, including strata-bound replacement ores and hydrothermal breccias. We use the implicit method to make a detailed three-dimensional geological model of a strata-bound IOCG in the Cloncurry District, the E1 Group...
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Journal Article
Journal: Economic Geology
Published: 01 March 2017
Economic Geology (2017) 112 (2): 397–422.
...Joao Babo; Carl Spandler; Nicholas H.S. Oliver; Mat Brown; Michael J. Rubenach; Robert A. Creaser Abstract The Merlin deposit, located in the Cloncurry district, Mt. Isa Inlier, is the world’s highest-grade Mo-Re deposit. Although the district is renowned for iron oxide copper-gold (IOCG)–type...
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Journal Article
Journal: Interpretation
Published: 29 July 2013
Interpretation (2013) 1 (1): T63–T84.
.... Schaltegger U. , 2001 The Osborne deposit, Cloncurry district: A 1595 Ma Cu–Au skarn deposit , in Williams P. J. , ed., 2001, a hydrothermal odyssey: Extended conference abstracts : James Cook University , 59, 58 – 59 . Geoscience Australia , 2010 , Surface geology of Australia, 1...
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Journal Article
Published: 01 July 2007
Exploration and Mining Geology (2007) 16 (3-4): 125–143.
... , 2006 ). Fig. 1. Location of Ernest Henry and other significant Cu-Au deposits in the Cloncurry mining district (Eastern Fold Belt, Mt. Isa block), with inset map of Australia. The dominant structural and geophysical grain at Ernest Henry strikes NE with lithological boundaries...
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Journal Article
Journal: Economic Geology
Published: 01 July 2001
Economic Geology (2001) 96 (4): 723–742.
... to be closer to the age of mineralization. The stage II biotite age of ca. 1521 Ma is interpreted to record thermal resetting during postore ductile deformation. The results suggest that micas in the Cloncurry district are more susceptible to later thermal resetting than amphiboles which may have significant...
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Journal Article
Journal: Economic Geology
Published: 01 July 2001
Economic Geology (2001) 96 (4): 875–883.
... . 1. Geologic setting of the Starra Au-Cu deposit. The Cloncurry district in the eastern Mount Isa block of northwest Queensland contains several significant Fe oxide-Cu-Au deposits ( Fig.1 ), which are similar in age but quite different in chemistry and geologic context from the very large...
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Journal Article
Published: 01 July 2001
Exploration and Mining Geology (2001) 10 (3): 191–213.
... Ma); the Gawler-Curnamona region (1640 Ma to 1590 Ma); and the Cloncurry district (Mount Isa Eastern Fold Belt, 1540 Ma to 1500 Ma with a possible earlier event at ca. 1600 Ma). No deposits are known to be coeval with various 1780 Ma to 1610 Ma anorogenic intrusions. Deposits are hosted by many...
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Journal Article
Journal: Economic Geology
Published: 01 August 2000
Economic Geology (2000) 95 (5): 1067–1089.
...., Geology of Australian and Papua New Guinean mineral deposits : Melbourne , Australasian Institute of Mining and Metallurgy , p. 793 – 799 . Baker , T. , 1998 , Alteration, mineralization and fluid evolution at the Eloise Cu-Au deposit, Cloncurry district, northwest Queensland, Australia...
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Journal Article
Journal: Economic Geology
Published: 01 December 1998
Economic Geology (1998) 93 (8): 1180–1189.
Journal Article
Journal: Economic Geology
Published: 01 December 1998
Economic Geology (1998) 93 (8): 1213–1236.
Journal Article
Journal: Economic Geology
Published: 01 December 1998
Economic Geology (1998) 93 (8): 1330–1344.
... and geochemical study of these granites in the southern part of the district have identified two groups of intrusions that are referred to here as the Cloncurry Supersuite and Eureka Supersuite.The Cloncurry Supersuite is composed mainly of monzogranite and syenogranite which consist of quartz, plagioclase...
Journal Article
Journal: Economic Geology
Published: 01 December 1998
Economic Geology (1998) 93 (8): 1390–1405.
...Lucy H. Chapman; Patrick J. Williams Abstract The Cannington deposit (47.3 million metric tons at 10.9% Pb, 4.3% Zn, and 490 g/t Ag) is hosted by sillimanite-K feldspar zone gneisses of the 1.67 Ga "Maronan supergroup" in the Mount Isa Eastern fold belt (Cloncurry mining district). Distinctive Fe...
Journal Article
Journal: Economic Geology
Published: 01 December 1998
Economic Geology (1998) 93 (8): 1435–1449.
...Jackie F. Rotherham; Kevin L. Blake; Ian Cartwright; Patrick J. Williams Abstract New stable isotope data are consistent with a metasomatic origin for the controversial Mesoproterozoic ironstone-hosted Au-Cu deposit at Starra in the Cloncurry district of northwest Queensland. This supports textural...
Journal Article
Published: 01 April 1997
Mineralogical Magazine (1997) 61 (2): 291–293.
Journal Article
Journal: Economic Geology
Published: 01 August 1993
Economic Geology (1993) 88 (5): 1114–1134.
...Patrick J. Williams; Maree Heinemann Abstract The significant but subeconomic (1.8 Mt4.4% Zn) Maramungee deposit is 90 km south-southeast of Cloncurry in northwest Queensland. It lies in the Eastern fold belt of the Proterozoic Mount Isa inlier within rocks of the Maronan Supergroup that also hosts...
Journal Article
Journal: Economic Geology
Published: 01 March 1957
Economic Geology (1957) 52 (2): 140–148.
Journal Article
Journal: Economic Geology
Published: 01 September 1956
Economic Geology (1956) 51 (6): 528–540.
Image
F ig  1. Regional geology of the <span class="search-highlight">Cloncurry</span> <span class="search-highlight">district</span> and Eloise Cu-Au deposi...
Published: 01 July 2001
F ig 1. Regional geology of the Cloncurry district and Eloise Cu-Au deposit locality map.
Image
Interpreted geological plan of the Ernest Henry deposit, <span class="search-highlight">Cloncurry</span> <span class="search-highlight">district</span>...
Published: 01 July 2001
Fig. 10. Interpreted geological plan of the Ernest Henry deposit, Cloncurry district. Simplified from Twyerould (1997) with geochronological data from Pollard and McNaughton (1997) and Gunton (1999) . Coordinate scheme is Australian Mapping Grid (UTM).
Image
Correspondence of Cu:Au ratios of <span class="search-highlight">Cloncurry</span> <span class="search-highlight">district</span> resources with variati...
Published: 01 July 2001
Fig. 20. Correspondence of Cu:Au ratios of Cloncurry district resources with variations in the assemblages of Fe phases that coexist with chalcopyrite in the ore. The distinct mineral associations of the Osborne western domain (W) and eastern high-grade (E) ore zones have been represented