Infrared spectroscopic measurements of glass inclusions within quartz
phenocrysts from the Plinian fallout of the 22 Ma tuff of Pine Grove (
southwestern Utah) show that the trapped silicate melt contained high
concentrations of H2O (6-8 wt%) and CO2 (60-960 ppm). Inclusion compos
itions are consistent with either open- or closed-system degassing of
this high-silica rhyolite during ascent from 16 km (430 MPa) to 9 km (
250 MPa) depth, prior to eruption. Intrusive porphyries from the Pine
Grove system are nearly identical in age, composition, and mineralogy
to the tephra, and some contain high-grade Mo mineralization. Assuming
that the porphyry magmas originally contained similar abundances of v
olatile components as the erupted rocks, they would have been saturate
d with fluid at pressures far greater than those at which the porphyri
es were emplaced and mineralized. Even if no initial exsolved fluid wa
s present when the magma began to ascend, it would have contained 19 t
o 39 vol% bubbles at the approximately 3 km depth (80 MPa) of emplacem
ent of many porphyries. The decrease in magma density and increase in
porosity would have facilitated magma convection as well as advection
of magmatic aqueous fluid through an interconnected network of bubbles
. The data are consistent with formation of Climax-type Mo porphyry de
posits by prolonged fluid flux from a large volume (> 20 km3) of relat
ively Mo-poor (1-5 ppm) magma.