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- W1987527418 abstract "Fluid inclusions in quartz from barren and Au-sulfide-bearing veins from the Cowra Creek Gold District, New South Wales, Australia, have been characterized based on their decrepitation behavior and gas geochemistry. Inclusions in Au-sulfide veins, and some regional sulfide-bearing veins, show distinctly higher CO2CH4 ratios compared to barren quartz-only and quartz-sulfid veins from the deposit environment. Additionally, the occurrence of low-temperature peaks in acoustic decrepigrams from Au-sulfide veins that had previously been attributed to the presence of CO2-bearing fluid inclusions has been confirmed using optical techniques. This characteristic peak is absent from quartz-sulfide and quartz-only veins. These results suggest that the gas content of fluid inclusions can distinguish Au-bearing from barren quartz veins, and that the acoustic decrepitation technique may provide a rapid and simple means of identifying different generations of quartz, and potentially productive veins in mesothermal environments." @default.
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- W1987527418 date "1995-11-01" @default.
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- W1987527418 title "Comparison of decrepitation, microthermometric and compositional characteristics of fluid inclusions in barren and auriferous mesothermal quartz veins of the Cowra Creek Gold District, New South Wales, Australia" @default.
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- W1987527418 doi "https://doi.org/10.1016/0375-6742(95)00031-3" @default.
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