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(A) The 18O and  13C compositions distinguish Mississippian age host (B) Variable 87Sr/86Sr composition indicates the precipitation of minerals did not rock from the most depleted values of this study that plot in the oval. all form simultaneously from the same fluid. The LMD samples reflect a Mm The depleted  13C of may reflect carbon derived from contamination Sr source while the PMD reflect Pennsylvanian-Permian hosted fluids likely with with hydrocarbons supporting mixing with basin derived fluids. Phosphoria Formation sourced hydrocarbons mixing with the Madison host rock.

abstracts with programs - geological society of america

URANIUM VANADIUM MINERALIZATION IN MISSISSIPPIAN AGED PALEOKARST, NORTHERN BIGHORN BASIN, MONTANA AND WYOMING, INDICATES A HYDROTHERMAL PERMIAN PHOSPHORIA FORMATION SOURCE OF METALS INCLUDING REE AND TL