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Volumn 284, Issue 5423, 1999, Pages 2159-2163

Gold solubility in supercritical hydrothermal brines measured in synthetic fluid inclusions

Author keywords

[No Author keywords available]

Indexed keywords

GOLD; HYDROGEN SULFIDE; IRON DERIVATIVE; MAGNETITE; SILICON DIOXIDE;

EID: 0033603395     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.284.5423.2159     Document Type: Article
Times cited : (240)

References (57)
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    • 2. The ice plus an annulus of quartz was laser-ablated and analyzed by ICPMS to simulate ablation and analysis of sealed fluid inclusions. Replicate analyses gave a mean (± 1 SD) U/Th = 5.8 [± 0.2), Au = 105 (± 11) ppm relative to Th, and Au = 107 (± 13) ppm relative to U as the internal standard. The 10 Au determinations gave a pooled mean of 106 ± 9 ppm Au at the 95% confidence limit From the pseudoinclusion tests, we conclude that (i) the analytical result 106 ± 9 ppm agrees with the nominal 103 ppm Au weighed into the standard solution, so no matrix-related bias is evident between the ablated glass standard and the ablated quartz + standard fluid, and (ii) in submicrogram-size samples, our analytical precision for Au by this U-Th dual-intemal-standard procedure is ±∼8% of the actual value.
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    • 2O expands with decreasing P or increasing T, narrowing the spacing of AuHS°(aq) solubility isobars.
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    • We thank S. Eggins, W. Hibberson, L. Kinsley, H. O'Neill, M. Shelley, and N. Ware for technical assistance in experimental and analytical aspects of this study and B. L. N. Kennett for supporting development of the analytical facilities. D. Ellis kindly shared his cold-seal laboratory. Comments by A. Berry, I. Campbell, C. Heinrich, S. Kesson, M. Palin, D. Sverjensky, and anonymous reviewers clarified the presentation.


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