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Structure, alteration, and geochemistry of the Charlotte quartz vein stockwork, Mt Charlotte gold mine, Kalgoorlie, Australia: Time constraints, down-plunge zonation, and fluid source Mineralium Deposita - Electronic Supplementary Material DOI 10.1007/s00126-014-0527-2 Accepted 11th of May 2014 Andreas G. Mueller Centre for Exploration Targeting, School of Earth and Environment, The University of Western Australia, 35 Stirling Highway, Crawley W.A. 6009, Australia E-mail: andreasm@iinet.net.au Table 1: Gold production from the Mt Charlotte area, Kalgoorlie district, Western Australia. Table 2: Quantitative X-ray diffraction mineralogy of altered Golden Mile Dolerite (GMD), Black Flag

greywacke, and hornblende porphyry, Mt Charlotte mine 22 level, Kalgoorlie. Table 3: Major and trace element analyses of Golden Mile Dolerite, porphyry and bulk gold ore

(channel + mill head) from the Mt Charlotte deposit, Kalgoorlie, Western Australia. Table 4: Major element analyses of metamorphosed and chlorite-carbonate altered Golden Mile

Dolerite versus bulk gold ore (mill head in 1985) from the Charlotte quartz vein orebody, Kalgoorlie, Western Australia.

Table 5: Trace element analyses of a pyrite flotation concentrate, the flotation tails, and the input mill head (May 21-27, 1978), Mt Charlotte gold deposit, Kalgoorlie.

Table 6: Rare earth element and Rb-Sr analyses of scheelite, Mt Charlotte gold deposit, Kalgoorlie, Western Australia.

Table 7: Scheelite, greenstone, and porphyry strontium and neodymium isotope data, Mt Charlotte gold deposit, Kalgoorlie.

Additional references in Tables Bateman, RJ, Costa S, Swe T, Lambert D (2001b) Archaean mafic magmatism in the Kalgoorlie area

of the Yilgarn Craton, Western Australia: a geochemical and Nd isotopic study of the petrogenetic and tectonic evolution of a greenstone belt. Precambrian Research 108: 75-112

Champion DC, Sheraton JW (1997) Geochemistry and Nd isotope systematics of Archaean granites of the Eastern Goldfields, Yilgarn Craton, Australia: implications for crustal growth processes. Precambrian Research 83: 109-132

Chauvel C, Dupré B, Jenner GA (1985) The Sm-Nd age of Kambalda volcanics is 500 Ma too old! Earth and Planetary Science Letters 74: 315-324

Cooper JA, Nesbitt RW, Platt JP, Mortimer GE (1978) Crustal development of the Agnew region, Western Australia, s shown by Rb/Sr and geochemical studies. Precambrian Research 7: 31-59

Deer WA, Howie RA, Zussman J (1992) The rock-forming minerals, 2nd edition. Longman Group UK, 696 p.

Hooton DH, Giorgetta NE (1977) Quantitative X-ray diffraction analysis by a direct calculation method: X-ray Spectrometry 6: 2-5

Keats W (1987) Regional geology of the Kalgoorlie-Boulder gold-mining district. Geological Survey of Western Australia, Perth, Report 21, 44 pp

Lee RF (1980) Simultaneous determination of carbon and sulphur in geological material using inductive combustion. Chemical Geology 31: 145-151

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Norrish K, Hutton JT (1969) An accurate X-ray spectrographic method for the analysis of a wide range of geological samples. Geochimica et Cosmochimica Acta 33: 431-453

Roddick JCM (1974) Responses of strontium isotopes to some crustal processes. Unpublished Ph.D. thesis, Australian National University, Canberra, 350 pp

Roddick JCM (1984) Emplacement and metamorphism of Archaean mafic volcanics at Kambalda, Western Australia – geochemical and isotopic constraints. Geochimica Cosmochimica Acta 48: 1305-1318

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