Research Paper THEMED ISSUE: Active Margins in Transition—Magmatism and Tectonics through Time: An Issue in Honor of Arthur W. Snoke GEOSPHERE Neoarchean tectonic history of the Teton Range: Record of accretion GEOSPHERE; v. 14, no. 3 against the present-day western margin of the Wyoming Province doi:10.1130/GES01559.1 B. Ronald Frost1, Susan M. Swapp1, Carol D. Frost1, Davin A. Bagdonas1,2, and Kevin R. Chamberlain1,3 1Department of Geology and Geophysics, University of Wyoming, Laramie, Wyoming 82071, USA 18 figures; 1 set of supplemental files 2Carbon Management Institute, University of Wyoming, Laramie, Wyoming 82071, USA 3Faculty of Geology and Geography, Tomsk State University, Tomsk 634050, Russia CORRESPONDENCE:
[email protected] ABSTRACT INTRODUCTION CITATION: Frost, B.R., Swapp, S.M., Frost, C.D., Bag- donas, D.A., and Chamberlain, K.R., 2018, Neoar- chean tectonic history of the Teton Range: Record Although Archean gneisses of the Teton Range crop out over an The Wyoming Province is an Archean craton that occupies most of of accretion against the present-day western margin area of only 50 × 15 km, they provide an important record of the Ar- Wyoming and portions of Montana, and adjacent states. The Archean rocks of the Wyoming Province: Geosphere, v. 14, no. 3, chean history of the Wyoming Province. The northern and southern are exposed in the cores of basement-involved Laramide uplifts. The early p. 1008–1030, doi:10.1130/GES01559.1. parts of the Teton Range record different Archean histories. The north- mafic crust appears to have been Hadean (Frost et al., 2017), though most of ern Teton Range preserves evidence of 2.69–2.68 Ga high-pressure the exposed area consists of Paleoarchean to Neoarchean quartzofeldspathic Science Editor: Shanaka de Silva Guest Associate Editor: Joshua Schwartz granulite metamorphism (>12 kbar, ~900 °C) followed by tectonic as- orthogneisses that retain an isotopic signature of that ancient crust (Frost, 1993).