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Golden Mile Deposit

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Journal Article

Synsedimentary to Early Diagenetic Gold in Black Shale-Hosted Pyrite Nodules at the Golden Mile Deposit, Kalgoorlie, Western Australia Available to Purchase

Jeffrey A. Steadman, Ross R. Large, Sebastien Meffre, Paul H. Olin, Leonid V. Danyushevsky, Daniel D. Gregory, Ivan Belousov, Elena Lounejeva, Trevor R. Ireland, Peter Holden
Journal: Economic Geology
Published: 01 August 2015
Economic Geology (2015) 110 (5): 1157–1191.
DOI: https://doi.org/10.2113/econgeo.110.5.1157
... telluride minerals, is a world-class Neoarchean Au-Ag-Te district, which includes the Golden Mile Super Pit, the largest single gold deposit in the Eastern Goldfields of Western Australia, and the smaller but nonetheless significant Mount Charlotte deposit, 3 km to the north. The gold ore at Kalgoorlie...
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View PDF for article title, Synsedimentary to Early Diagenetic Gold in Black Shale-Hosted Pyrite Nodules at the <span class="search-highlight">Golden</span> <span class="search-highlight">Mile</span> <span class="search-highlight">Deposit</span>, Kalgoorlie, Western Australia
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Journal Article

The Age of the Giant Golden Mile Deposit, Kalgoorlie, Western Australia: Ion-Microprobe Zircon and Monazite U-Pb Geochronology of a Synmineralization Lamprophyre Dike Available to Purchase

Neal J. McNaughton, Andreas G. Mueller, David I. Groves
Journal: Economic Geology
Published: 01 November 2005
Economic Geology (2005) 100 (7): 1427–1440.
DOI: https://doi.org/10.2113/gsecongeo.100.7.1427
...Neal J. McNaughton; Andreas G. Mueller; David I. Groves Abstract Open-pit and underground mines in the Golden Mile at Kalgoorlie, Western Australia, have produced more than 1,475 metric tons (t) of gold since 1893. Despite the economic importance of the deposit, the age of the mineralized shear...
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View PDF for article title, The Age of the Giant <span class="search-highlight">Golden</span> <span class="search-highlight">Mile</span> <span class="search-highlight">Deposit</span>, Kalgoorlie, Western Australia: Ion-Microprobe Zircon and Monazite U-Pb Geochronology of a Synmineralization Lamprophyre Dike
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Journal Article

TELLURIDE MINERALOGY OF THE GOLDEN MILE DEPOSIT, KALGOORLIE, WESTERN AUSTRALIA Available to Purchase

Jill M. Shackleton, Paul G. Spry, Roger Bateman
Published: 01 December 2003
The Canadian Mineralogist (2003) 41 (6): 1503–1524.
DOI: https://doi.org/10.2113/gscanmin.41.6.1503
...). Nineteen tellurium-bearing minerals occur in the Golden Mile deposit. Calaverite, petzite, coloradoite, altaite and native gold are most common throughout the deposit, whereas tellurantimony, melonite, hessite, stützite, krennerite and sylvanite are rare in the main and caunter lodes. In addition, hessite...
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View PDF for article title, TELLURIDE MINERALOGY OF THE <span class="search-highlight">GOLDEN</span> <span class="search-highlight">MILE</span> <span class="search-highlight">DEPOSIT</span>, KALGOORLIE, WESTERN AUSTRALIA
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Journal Article

The Golden Mile, Kalgoorlie; a giant gold deposit localized in ductile shear zones by structurally induced infiltration of an auriferous metamorphic fluid Available to Purchase

C. A. Boulter, M. G. Fotios, G. Neil Phillips
Journal: Economic Geology
Published: 01 November 1987
Economic Geology (1987) 82 (7): 1661–1678.
DOI: https://doi.org/10.2113/gsecongeo.82.7.1661
... geometrically to the three ductile shear zones. Golden Mile-style mineralization is syntectonic and was not deposited posttectonically in structurally prepared sites. Microtextural analysis demonstrates that minerals associated with gold emplacement are strongly modified during strain within the ductile shear...
View PDF for article title, The <span class="search-highlight">Golden</span> <span class="search-highlight">Mile</span>, Kalgoorlie; a giant gold <span class="search-highlight">deposit</span> localized in ductile shear zones by structurally induced infiltration of an auriferous metamorphic fluid
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Journal Article

Host rock and fluid control on carbonate assemblages in the Golden Mile Dolerite, Kalgoorlie gold deposit, Australia Available to Purchase

G. Neil Phillips, Isobel J. Brown
Published: 01 June 1987
The Canadian Mineralogist (1987) 25 (2): 265–273.
View PDF for article title, Host rock and fluid control on carbonate assemblages in the <span class="search-highlight">Golden</span> <span class="search-highlight">Mile</span> Dolerite, Kalgoorlie gold <span class="search-highlight">deposit</span>, Australia
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Structural map of the Golden Mile deposit (modified from Mueller et al., 1988), showing the locations of the Paringa South shaft and the Oroya lode in the eastern part of the Fimiston shear zone system. The Fimiston lodes occupy brittle shear zones subsidiary to the sinistral Golden Mile (GMF) and Boulder-Lefroy (BLF) faults, which displace upright regional folds such as the Kalgoorlie anticline. The sinistral faults are offset by the Golden Pike fault (GPF), the Adelaide fault (ADF), and by other dextral faults.

Structural map of the Golden Mile deposit (modified from Mueller et al., 1... Available to Purchase

Published: 01 November 2005
F ig . 2. Structural map of the Golden Mile deposit (modified from Mueller et al., 1988 ), showing the locations of the Paringa South shaft and the Oroya lode in the eastern part of the Fimiston shear zone system. The Fimiston lodes occupy brittle shear zones subsidiary to the sinistral Golden
Image
Photograph of the dated lamprophyre dike in the Golden Mile deposit, Paringa South shaft, level 6, looking northeast. The dark-gray dike, altered to a chlorite-carbonate-quartz assemblage, cuts across sericite-ankerite–altered Paringa pillow basalt in the footwall of the Oroya shear zone (from Mueller et al., 1988).

Photograph of the dated lamprophyre dike in the Golden Mile deposit, Paring... Available to Purchase

Published: 01 November 2005
F ig . 3. Photograph of the dated lamprophyre dike in the Golden Mile deposit, Paringa South shaft, level 6, looking northeast. The dark-gray dike, altered to a chlorite-carbonate-quartz assemblage, cuts across sericite-ankerite–altered Paringa pillow basalt in the footwall of the Oroya shear
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Geological map of the Golden Mile deposit showing the location of the “Super Pit” and thirteen of the lodes sampled during this study (A2: Associated #2, AE: Australia East #3, B: B, BA: Blatchford, BO: Boulder, E: Emerald, F: Furness, LV: Lake View – Main, N3: No. 3 Western, N4: No. 4 Western, O: Oroya, P: Perseverance, T: Tetley).

Geological map of the Golden Mile deposit showing the location of the “Supe... Available to Purchase

Published: 01 December 2003
F ig . 2. Geological map of the Golden Mile deposit showing the location of the “Super Pit” and thirteen of the lodes sampled during this study (A2: Associated #2, AE: Australia East #3, B: B, BA: Blatchford, BO: Boulder, E: Emerald, F: Furness, LV: Lake View – Main, N3: No. 3 Western, N4: No. 4
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Paragenetic sequence of Fimiston-style ores at the Golden Mile deposit (modified after Clout 1989).

Paragenetic sequence of Fimiston-style ores at the Golden Mile deposit (mod... Available to Purchase

Published: 01 December 2003
F ig . 3. Paragenetic sequence of Fimiston-style ores at the Golden Mile deposit (modified after Clout 1989 ).
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REPRESENTATIVE COMPOSITIONS OF TELLURIDES GOLDEN MILE DEPOSIT Available to Purchase

Published: 01 December 2003
TABLE 3. REPRESENTATIVE COMPOSITIONS OF TELLURIDES GOLDEN MILE DEPOSIT
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Maps of the Golden Mile deposit illustrating the location of: (A) calaverite, montbrayite and krennerite, (B) petzite and sylvanite, (C) hessite and stützite, (D) altaite, coloradoite and tellurantimony. Data are from Golding (1978) and this study.

Maps of the Golden Mile deposit illustrating the location of: (A) calaverit... Available to Purchase

Published: 01 December 2003
F ig . 10. Maps of the Golden Mile deposit illustrating the location of: (A) calaverite, montbrayite and krennerite, (B) petzite and sylvanite, (C) hessite and stützite, (D) altaite, coloradoite and tellurantimony. Data are from Golding (1978) and this study.
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The stabilities of sulfides and tellurides in the Golden Mile deposit as a function of f(S2) and f(Te2). (A) Early stage 3 (shaded area), (B) late stage 3 (shaded area). Although petzite – sylvanite and sylvanite – hessite formed below 170°C from reactions involving γ-phase or χ-phase (Cabri 1965), only the stability of hessite is shown here in view of the thermodynamic data available. Equilibria were calculated at 100°C using data listed in Afifi et al.(1988).

The stabilities of sulfides and tellurides in the Golden Mile deposit as a ... Available to Purchase

Published: 01 December 2003
F ig . 11. The stabilities of sulfides and tellurides in the Golden Mile deposit as a function of f (S 2 ) and f (Te 2 ). (A) Early stage 3 (shaded area), (B) late stage 3 (shaded area). Although petzite – sylvanite and sylvanite – hessite formed below 170°C from reactions involving γ-phase
Journal Article

A New Geochemical Technique for Gold Exploration: Alkali Element Mobility Associated with Gold Mineralization in the West Australian Goldfields Available to Purchase

Christopher J. Heath, Ian H. Campbell
Journal: Economic Geology
Published: 01 March 2004
Economic Geology (2004) 99 (2): 313–324.
DOI: https://doi.org/10.2113/gsecongeo.99.2.313
... samples of two mafic rock types from four localities in the Archean Yilgarn craton of Western Australia; the giant Golden Mile deposit at Kalgoorlie, the smaller Victory mine at Kambalda, two drill holes that intersected subeconomic mineralization 8 km south of Kalgoorlie, and two drill holes well away...
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View PDF for article title, A New Geochemical Technique for Gold Exploration: Alkali Element Mobility Associated with Gold Mineralization in the West Australian Goldfields
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Journal Article

40 Ar- 39 Ar and U-Pb age constraints on the timing of gold mineralization in the Kalgoorlie gold field, Western Australia Available to Purchase

A. J. R. Kent, I. McDougall
Journal: Economic Geology
Published: 01 July 1995
Economic Geology (1995) 90 (4): 845–859.
DOI: https://doi.org/10.2113/gsecongeo.90.4.845
... ). At the nearby Golden Mile deposit 40 Ar- 39 Ar ages from two muscovite samples associated with shear-hosted lode gold mineralization have a weighted mean of 2629 + or - 9 Ma. On the balance of available evidence these ages are interpreted to represent the timing of gold mineralization in the two deposits.These...
View PDF for article title, 40 Ar- 39 Ar and U-Pb age constraints on the timing of gold mineralization in the Kalgoorlie gold field, Western Australia
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Journal Article

No mass-independent sulfur isotope fractionation in auriferous fluids supports a magmatic origin for Archean gold deposits Available to Purchase

Yunxing Xue, Ian Campbell, Trevor R. Ireland, Peter Holden, Richard Armstrong
Journal: Geology
Published: 01 July 2013
Geology (2013) 41 (7): 791–794.
DOI: https://doi.org/10.1130/G34186.1
... to the gold mineralization from the Bellerophon, Victory, and Wallaby deposits in the Eastern Goldfield superterrane of the Yilgarn craton, Western Australia, together with sulfide from black shale from the Golden Mile deposit and St. Ives gold camp. Ore-associated pyrite from the Beattie gold deposit...
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View PDF for article title, No mass-independent sulfur isotope fractionation in auriferous fluids supports a magmatic origin for Archean gold <span class="search-highlight">deposits</span>
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F ig . 7. Primitive mantle normalized trace element plots of Golden Mile Do... Available to Purchase

Published: 01 March 2004
F ig . 7. Primitive mantle normalized trace element plots of Golden Mile Dolerite. The dolerite from the Golden Mile deposit (a) exhibits stronger alkali enrichment than the dolerite from subeconomic mineralization in drill holes DDH SE-10 and DDH SE-12 (b).
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F ig . 9. Histogram of ((Cs + Rb)/Th) N ratios for samples of the Golden M... Available to Purchase

Published: 01 March 2004
F ig . 9. Histogram of ((Cs + Rb)/Th) N ratios for samples of the Golden Mile Dolerite from the Golden Mile and drill holes DDH SE-10 and DDH SE-12. Samples proximal to the giant Golden Mile deposit (a) have higher ((Cs + Rb)/Th) N than those associated with the subeconomic gold mineralization
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REPRESENTATIVE COMPOSITIONS OF PYRITE AND TETRAHEDRITE-GROUP MINERALS, GOLD... Available to Purchase

Published: 01 December 2003
TABLE 1. REPRESENTATIVE COMPOSITIONS OF PYRITE AND TETRAHEDRITE-GROUP MINERALS, GOLDEN MILE DEPOSIT
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TELLURIDE AND NATIVE ELEMENT CONTACT-ASSEMBLAGES DOCUMENTED FOR THE GOLDEN ... Available to Purchase

Published: 01 December 2003
TABLE 4. TELLURIDE AND NATIVE ELEMENT CONTACT-ASSEMBLAGES DOCUMENTED FOR THE GOLDEN MILE DEPOSIT
Journal Article

Source requirements for the Golden Mile, Kalgoorlie: significance to the metamorphic replacement model for Archean gold deposits Free

G. Neil Phillips, David I. Groves, Isobel J. Brown
Published: 01 August 1987
Canadian Journal of Earth Sciences (1987) 24 (8): 1643–1651.
DOI: https://doi.org/10.1139/e87-158
... providing focussing of fluids and multiple channelways through specific Fe-rich, low-tensile-strength host rocks to ensure efficient depositional mechanisms. Le gîte de Golden Mile, à Kalgoorlie, représente un vaste système aurifère hydrothermal d'âge archéen localisé dans les zones de cisaillement...
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