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Agnew-Wiluna greenstone belt

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Journal Article
Journal: Economic Geology
Published: 01 August 2012
Economic Geology (2012) 107 (5): 781-796.
...Marco Fiorentini; Steve Beresford; Mark Barley; Paul Duuring; Andrey Bekker; Nic Rosengren; Ray Cas; Jon Hronsky Abstract The Agnew-Wiluna greenstone belt of Western Australia is the largest komatiite-hosted nickel sulfide belt in the world and contains two world-class Ni-Cu-(PGE) deposits...
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Geologic map of the <b>Agnew</b>-<b>Wiluna</b> <b>greenstone</b> <b>belt</b> simplified after  Beresfor...
Published: 01 August 2012
Fig. 1 Geologic map of the Agnew-Wiluna greenstone belt simplified after Beresford et al. (2004) . The structural domains discussed in the main text are shown in bold format, whereas names of key localities are indicated in small boxes.
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Simplified geologic map of the <b>Agnew</b>-<b>Wiluna</b> <b>greenstone</b> <b>belt</b>, Western Austra...
Published: 01 March 2008
F ig . 2. Simplified geologic map of the Agnew-Wiluna greenstone belt, Western Australia (adapted from Hill et al., 1990 ). The boxes show the setting of the localities from where samples were collected. CLU = Cliffs ultramafic unit, MKU = Mount Keith ultramafic unit.
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Simplified geologic map of the <b>Agnew</b>-<b>Wiluna</b> <b>greenstone</b> <b>belt</b> in the Eastern ...
Published: 01 March 2007
F ig . 1. Simplified geologic map of the Agnew-Wiluna greenstone belt in the Eastern Goldfields province of Western Australia, showing the location of the Leinster camp nickel sulfide deposits along the eastern margin of the belt and proximal to the north-northwest–trending Mount Keith-Kilkenny
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Geological map of the Mt Keith area, <b>Agnew</b>–<b>Wiluna</b> <b>Greenstone</b> <b>Belt</b>, showing ...
Published: 01 November 2001
Fig. 2. Geological map of the Mt Keith area, AgnewWiluna Greenstone Belt, showing distribution of olivine–adcumulate, olivine–mesocumulate filled lava pathways and flanking olivine orthocumulate and spinifex-textured flow units, Flood Flow Facies II (after Dowling & Hill 1993).
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Geology of part of the <b>Agnew</b>–<b>Wiluna</b> <b>Greenstone</b> <b>Belt</b> showing the distributio...
Published: 01 November 2001
Fig. 1. Geology of part of the AgnewWiluna Greenstone Belt showing the distribution of komatiite rocks and the location of MKD5 and other significant Ni sulphide mines.
Image
Geology of part of the <b>Agnew</b>–<b>Wiluna</b> <b>Greenstone</b> <b>Belt</b> showing the distributio...
Published: 01 November 2001
Fig. 1. Geology of part of the AgnewWiluna Greenstone Belt showing the distribution of komatiite rocks and the location of MKD5 and other significant Ni sulphide mines.
Image
Geological map of the Mt Keith area, <b>Agnew</b>–<b>Wiluna</b> <b>Greenstone</b> <b>Belt</b>, showing ...
Published: 01 November 2001
Fig. 2. Geological map of the Mt Keith area, AgnewWiluna Greenstone Belt, showing distribution of olivine–adcumulate, olivine–mesocumulate filled lava pathways and flanking olivine orthocumulate and spinifex-textured flow units, Flood Flow Facies II (after Dowling & Hill 1993).
Journal Article
Journal: Economic Geology
Published: 01 May 1988
Economic Geology (1988) 83 (3): 524-536.
...Stephen J. Barnes; Martin J. Gole; Robin E. T. Hill Abstract The Agnew (formerly Perseverance) nickel deposit, in the Agnew-Wiluna greenstone belt of the Yilgarn block, has previously been assigned to the category of intrusive dunite-associated deposits. On the basis of detailed reinterpretation...
Journal Article
Journal: Economic Geology
Published: 01 March 2007
Economic Geology (2007) 102 (2): 277-297.
...F ig . 1. Simplified geologic map of the Agnew-Wiluna greenstone belt in the Eastern Goldfields province of Western Australia, showing the location of the Leinster camp nickel sulfide deposits along the eastern margin of the belt and proximal to the north-northwest–trending Mount Keith-Kilkenny...
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Series: Special Publications of the Society of Economic Geologists
Published: 01 January 2006
DOI: 10.5382/SP.13.04
EISBN: 9781629490373
... and Goliath North), discovered over the 1970 to 1971 period, are being evaluated at the time of writing. Both groups of deposits occur within the Archean Agnew-Wiluna greenstone belt and are hosted in giant olivine cumulate ultramafic bodies interpreted to be subsea-floor intrusions in a felsic...
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Journal Article
Journal: Economic Geology
Published: 01 March 2015
Economic Geology (2015) 110 (2): 469-503.
... in three dimensions has played a significant part in the recent discovery of the Venus deposit. The Leinster nickel camp is situated toward the southern end of the Agnew-Wiluna Belt ( Fig. 1 ). The Agnew-Wiluna Belt greenstone succession can be divided into an older (>2736 Ma) sequence...
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Journal Article
Journal: Economic Geology
Published: 01 August 2016
Economic Geology (2016) 111 (5): 1159-1185.
... stratigraphy and the gravity response and can be used to divide the Agnew-Wiluna belt into rift segments. The third set of early structures trends NNE, subparallel with the volcanic grain of the greenstones as inferred from the orientation of komatiite lava pathways. These are thought to have originated...
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Journal Article
Journal: Economic Geology
Published: 01 November 2015
Economic Geology (2015) 110 (7): 1669-1695.
...Caroline S. Perring Abstract The Mount Keith region of the Agnew-Wiluna belt in Western Australia is perhaps best known for hosting the giant komatiite-associated disseminated Ni sulfide deposit known as MKD5. It also hosts the sizeable Cliffs massive Ni sulfide deposit, which is the eighth largest...
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Series: Reviews in Economic Geology
Published: 01 January 2011
DOI: 10.5382/Rev.17.02
EISBN: 9781629490243
...: the Kambalda domain in the south, containing the deposits of the Kambalda-St Ives-Tramways trend and the Widgiemooltha dome; and the Agnew-Wiluna greenstone belt in the north. The term "Kalgoorlie terrane" replaces the now obsolete, but formerly widely used designation "Norseman-Wiluna greenstone belt...
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Regional geology of the <b>Agnew</b>-<b>Wiluna</b> <b>Belt</b> (AWB; adapted from  Beresford et ...
Published: 01 March 2015
Fig. 1 Regional geology of the Agnew-Wiluna Belt (AWB; adapted from Beresford et al., 2004 ). The inset of the Yilgarn craton shows granite-gneiss terrains in light gray and greenstones in darker gray: greenstones of the Kalgoorlie terrane are highlighted in charcoal gray.
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Regional geologic map of the <b>Agnew</b>-<b>Wiluna</b> <b>belt</b> (adapted from  Beresford et ...
Published: 01 August 2016
Fig. 1 Regional geologic map of the Agnew-Wiluna belt (adapted from Beresford et al., 2004 ), showing the location of the Yakabindie three-dimensional model in relationship to the Leinster and Mount Keith models. The inset of the Yilgarn craton shows granite-gneiss terranes in light gray
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Regional geology of the <b>Agnew</b>-<b>Wiluna</b> <b>belt</b> (AWB; adapted from  Beresford et ...
Published: 01 November 2015
Fig. 1 Regional geology of the Agnew-Wiluna belt (AWB; adapted from Beresford et al., 2004 ). The inset of the Yilgarn craton shows granite-gneiss terranes in light gray and greenstones in darker gray. Greenstones of the Kalgoorlie, Kurnalpi, and Burtville terranes (which collectively make up
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Simplified stratigraphic sections in selected domains of the <b>Agnew</b>-<b>Wiluna</b> g...
Published: 01 August 2012
Fig. 2 Simplified stratigraphic sections in selected domains of the Agnew-Wiluna greenstone belt (cf. Fig. 1 ). The architecture of the Mount Keith Domain is the location where the stratigraphic relationships within the greenstone belt are best preserved. The Mount Keith Domain contains three
Journal Article
Journal: Economic Geology
Published: 01 November 2013
Economic Geology (2013) 108 (7): 1731-1752.
... example but other bodies are present in the Agnew-Wiluna greenstone belt such as Mount Clifford-Marshall Pool, Perseverance, Yakabindie, and Honeymoon Well ( Hill et al., 1995 ). The lenticular bodies host some of the largest known low-grade nickel sulfide orebodies found in komatiites ( Barnes, 2006a...
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