Southeastern Section - 57th Annual Meeting (10–11 April 2008)

Paper No. 15
Presentation Time: 8:00 AM-12:00 PM


WARREN, D. Morgan, COLLINS, Christin R., BRODA, Cindi, DAVARPANAH, Armita, DICKIE, Jennifer, REINSHAGEN, Mandi, SMUCYGZ, Barbara, VAN TREES, Craig, WOODWARD, Michael and KROGSTAD, Eirik, Geosciences, Georgia State University, P.O. Box 4105, Atlanta, GA 30302,

Although zircon U-Pb ages of N. American Cambrian sandstones have been studied extensively, little is known about the zircons in units in the northwestern United States (Flathead Sandstone). We determined zircon U-Pb ages in the Flathead Sandstone in the W. Highland Range at Camp Creek (S.W. Montana), where it locally overlies gneisses and amphibolites, thought to be late Archean or early Proterozoic. Here the Flathead Sandstone is ~20 m thick and it is deposited on a distinct paleosol. Two Flathead samples were studied, one of the lowermost 10 cm, one of the uppermost 30 cm. Forty-nine grains from each sample were analyzed by LA-ICP-MS. The largest grouping of grains from the upper sample have 207Pb/206Pb ages of 1.9-1.7 Ga (39%). In this sample there is one concordant or nearly concordant grain of late Archean 207Pb/206Pb age. The oldest 207Pb/206Pb ages are 2 grains at ~3.18 Ga. These zircon ages compare well with zircon age populations in quartzites of the Missoula Group (Belt Supergroup) (Ross and Villeneuve, 2002). Zircons from the lower sample are strikingly different. Here 16% of the grains have 207Pb/206Pb ages greater than 3.18 Ga, ranging up to 3.46 Ga. The lower sample may reflect partial derivation from the immediately underlying basement, the zircons in the upper sample may be more representative of detritus derived from the Belt Supergroup. These results for the lower sample would tend to support the suggestion by Gunn (1991, unpublihsed, Ph.D dissertation) that gneisses in the southern highland range include middle Archean components.