Joint 70th Rocky Mountain Annual Section / 114th Cordilleran Annual Section Meeting - 2018

Paper No. 11-6
Presentation Time: 8:30 AM-6:30 PM

PETROGRAPHICALLY-LINKED, GEOCHRONOLOGIC EVIDENCE FOR WIDESPREAD CA. 1.6 GA DEFORMATION IN THE NORTHERN COLORADO PALEOPROTEROZOIC CRUST: METHODS AND EXAMPLES


CUBRICH, Bart T., Geology/Geophysics, UniversityWyoming, 6001 Dodge St, Laramie, WY 82070, CHAMBERLAIN, Kevin R., Dept. of Geology and Geophysics, University of Wyoming, Dept. 3006, 1000 University Avenue, Laramie, WY 82071, DUEBENDORFER, Ernest, Department of Geology, Northern Arizona Univ, Flagstaff, AZ 86011, WILLIAMS, Michael, Geosciences, Univ of Massachusetts, 611 N. Pleasant St, Amherst, MA 01003 and HAMLIN, Jeffre W., Civil Engineering, Northern Arizona University, Flagstaff, AZ 86011

This poster presents the results of detailed field mapping, petrology, and kinematically-linked geochronology from five shear zones in Colorado with emphasis on the Soda Creek-Fish Creek shear zone (SCFCSZ) in Routt National Forest, Colorado, and the Kings Canyon mylonite near Walden, CO. The SCFCSZ records at least two periods of deformation: 1) a higher temperature ductile phase up to feldspar plasticity at ~1.68 Ga, and 2) a lower temperature brittle phase with epidote growth and formation of cataclasites at ~1.60 Ga (e.g., Hamlin, 2013; Duebendorfer et al., 2015; Cubrich et al., 2016; Cubrich, 2017). The Kings Canyon mylonite records an upper greenschist grade in the form of Epidote + Quartz + Chlorite + Actinolite pinstripe mylonites with epidote and titanite deformational ages that range from ~1.65-1.55 Ga. This study presents U-Pb data from multiple periods of metamorphic growth of titanite and monazite that directly date SCFCSZ activity/deformation from 1.77-1.57 Ga, but focuses on textural relations and the reaction mechanisms that led to the formation of these mylonites/shear zones. Our data suggest at least 5 periods of tectonism for the region: 1.77 Ga regional accretionary fabrics (tightly constrained at 1774±2 Ma in SCFCSZ); an event at 1.72-1.70 Ga, with unknown tectonic significance (SCFCSZ); at least two periods of high strain reactivation, ca. 1.66 and 1.60 Ga (SCFCSZ and Kings Canyon); and 1.42 Ga plutonism. The compilation of new geochronology and structural data from these shear zones add to a growing body of data that document a major period of regional tectonism at 1.65-1.55 Ga, well inboard from the active accretionary margin, with breakout, foreland thrusts concentrated in the lithosphere west of a N-S 1.68-1.60 Ga transform fault.
Handouts
  • Cubrich et al. (2018) Poster, 5-10-18.pdf (9.0 MB)