Noble gas composition of deep brines from the Palo Duro Basin, Texas

Mathematics – Logic

Scientific paper

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Scientific paper

Deep groundwaters in sedimentary basins can be sufficiently old (> 10 m.y.) to have accumulated both radiogenic 4 He and 40 Ar * . Differences in the ratio of( U + Th )/ K for aquifer lithologies lead to variations for 4 He / 40 Ar * in the groundwater. These variations can be used to resolve chronologically significant noble gas components. Application of a binary model to brine samples from the Palo Duro Basin, Texas yields (U, Th)- 4 He residence times of 100 to 300 m.y. Concentrations of two non-radiogenic noble gases ( 20 Ne and 36 Ar) provide information on the salinities of the water that recharged these aquifers.

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