The Carlin-type disseminated gold orebodies of Yankee basin in the southern
part of the Alligator Ridge mining district in Nevada contain widespread o
il as smears, open-space fillings, and fluid inclusions in syn- and pre-min
eral calcite veins. These unusual oils are the relicts of an exhumed and de
eply oxidized oil reservoir that encompasses the orebodies at the crest of
a dissected, anticlinal trap. Results of fluid-inclusion microthermometry a
nd organic geochemistry demonstrate that the oils experienced peak paleotem
peratures of no more than about 150 degrees C, a temperature unusually low
for Carlin-type mineralization, but ideal for the transport, entrapment, an
d preservation of liquid hydrocarbon. Similar geothermal systems are active
ly circulating at three of Nevada's producing oilfields-Grant Canyon, Bacon
Flat, and Blackburn. Accordingly, concealed Carlin-type fossil hydrotherma
l systems of this type even if subeconomic for gold, could contain commerci
al concentrations of oil.