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- W856876589 abstract "Fluid inclusion and wall rock alteration data from the Sixteen-toOne deposit indicate precious metals precipitated in response to temperature decrease resulting from fluid mixing and boiling. Fluid temperatures and salinities varied from 145° to 225°C and from 3.5 to 11.5 wt% NaCl equivalent, respectively; fluids decrease an average of 40°C and 1.4 wt% NaCl equivalent over an elevation increase of 130 meters. Homogenization temperatures and salinities become more variable in upper levels coincident with increased precious metal abundances. Fluids contained variable amounts of COz. Fracturing and open space filling are the most important wall rock changes produced by the hydrothermal event; metasomatism is minor. Vein-controlled alteration minerals include primarily quartz with lesser calcite, chlorite, pyrite, adularia, epidote, and montmorillonite, and trace white micas; zoning is typical of that present in active geothermal systems. Observed enthalpy-chloride relationships are consistent with mixing of deep, 225°C fluids and shallow, 93°C fluids." @default.
- W856876589 created "2016-06-24" @default.
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- W856876589 date "1986-01-01" @default.
- W856876589 modified "2023-09-23" @default.
- W856876589 title "The sixteen-to-one epithermal silver-gold deposit, Esmeralda County, Nevada: a wall rock alteration and fluid inclusion study" @default.
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