Augustine dome-3 gas. Symonds et al., 1990. Bull. Volcanol. 52, 355-374.
No trace elements in this run.  GASRUN Demonstration 1.

<  ERPC  >< FO2log ><  UNACT >< GASTOT ><  tempC ><   PF   ><   RAT  >
.10000E-110.0000E+00.00000E+00.10000E+01.87000E+03.10000E+01-.3000E+03

 BSTO NTEM NMTT NMOL IGAM NLOO NSUN IPRI ITRE
   42    0    1    0    0   90    0    0    0

<saq> < name >    <     mtot     ><     mtry     ><  gamma >
    1 H2           -.169100000E+00 0.500000000E-02  1.0000
    2 H2O          0.953300000E+00 0.800000000E+00  1.0000
    3 CO2          0.242000000E-01 0.200000000E-01  1.0000
    4 H2S          0.712000000E-01 0.100000000E-01  1.0000
    5 HCl          0.604000000E-01 0.600000000E-01  1.0000
    6 HF           0.860000000E-03 0.800000000E-02  1.0000



Symonds et al., 1990 is proably this:

Symonds, R.B., Rose, W.I., Gerlach, T.M., Briggs, P.H., and Harmon, R.S. (1990)
Evaluation of gases, condensates, and SO2 emissions from Augustine volcano, Alaska:
The degassing of a Cl- rich volcanic system. Bull. Volcanol. 52, 355-374.


The dome-3 data is quite likely identical to the GCA paper:

Symonds, R.B., Reed, M.H., Rose, W.I., 1992. Origin, speciation, and fluxes of
trace-element gases at Augustine volcano, Alaska: Insights into magma degassing
and fumarolic processes. Geochim. Cosmochim. Acta 56, 633-657.
Table 1 page 636 shows trace and major gases in separate blocks.