“…The fluid-inclusion evidence for the region is mixed; boiling is indicated in some deposits but not in others. However, boiling may not be evident in fluid inclusions if the gas-rich fluid was not trapped (Saunders and Rowan, 1986), and Henley (1985) noted that boiling is virtually inevitable as geothermal water rises to shallow depths; thus boiling is likely on geologic grounds for Tertiary systems of the Tonopah quadrangle. The major effects of boiling on the chemistry of epithermal fluids (Buchanan, 1981;Reed and Spycher, 1985;Hedenquist, 1991) must be considered to have been important in the Tertiary systems of the Tonopah region.…”