FISSION-TRACK EVIDENCE OF LATE TERTIARY COOLING AND INCISION OF THE WIND RIVER BASIN, WYOMING
Laramide cooling ages are widely reported from ranges surrounding the Wind River Basin, however they dont show evidence for post-Laramide uplift. Perched remnants of Tertiary tuffaceous deposits in the region as well as vitrinite reflectance data from the basin suggest that 1 to 3 km of post-Laramide basin fill was present, consistent with our fission-track results. The implication is that maximum burial, and hence heating, was post-Laramide in age and predates final exhumation of the basin. The younger break in slope indicates when final exhumation and cooling of the area began.
These results are consistent with those of published fission-track studies from the northern Green River Basin and the Powder River Basin also in the central Rockies that indicate post-Laramide (Miocene-Pliocene) final cooling. Up to 1 km of erosion has taken place in both of these basins, since ~4 Ma in the northern Green River Basin and since ~12 Ma in the southern Powder River Basin. The thermal history outlined here supports the view that significant incision of the central Rocky Mountains took place beginning in late Miocene or younger time, not dissimilar to the inferred history of Colorado Plateau to the south.