REGIONAL HELIUM ACCUMULATION GEOCHEMISTRY, LA BARGE PLATFORM, WYOMING
Gas and water samples from six Mississippian producing gas wells and 17 gas-effusive springs were collected for chemical analysis from 2012 to 2016. Gas-effusive springs within a 200 km radius of La Barge were sampled during the same period. Water and gas samples from all locations were analyzed for composition, major and trace element concentrations, and stable and noble gas isotopes.
Helium and other noble gas isotope results from the samples indicate three distinct regional helium source groups that roughly match the three major geologic provinces in the region. The first is the tectonically stable sedimentary strata of the La Barge Platform region; results here suggest the helium has crustal origins and helium concentrations are relatively high. The helium of this group is not however purely crustal and appears to represent an unknown end member with R/RA ratios of 0.05 to 0.07. The second group occurs to the west of La Barge in south eastern Idaho’s Basin and Range province. Here, there is more mantle-type helium with R/RA values of 0.15-2.2 and at lower concentrations than the first region. The last group, the Yellowstone region to the north, is well documented in the literature with mantle type helium. This area was only tangentially sampled for this study. Overall, the higher concentrations of helium occur in the sedimentary La Barge Platform region samples and they are isotopically of more crustal origin than the samples from the other regions. High helium concentration gases at surface springs in this region suggest that additional, potentially economic reservoirs of the gas are present.