T37 Deformation Localization throughout the Crust (Posters)

Sunday, 19 October 2014
9:00 AM - 5:00 PM
Exhibition Hall C

PRELIMINARY INVESTIGATION OF THE FOOTWALL TRANSITION OF THE BORREGO SPRINGS SHEAR ZONE

Paper number: T37-11
Program: Technical Sessions
Time: 9:00 AM – 5:00 PM

Authors

  • M.J. Vadman Presenting Author
    California State Polytechnic University, Pomona, Pomona, CA

Abstract

The Borrego Springs Shear Zone in the Peninsular Range Batholith, California, is an east over west thrusting regime that is part of the Eastern Peninsular Ranges Mylonite Zone. To the west, undeformed tonalite is dominant. Moving east, tonalite becomes foliated and mylonitized in places. Further east, the full transition to the footwall is unclear as it is covered by Quaternary deposits. While roughly continuous on a regional level, there is no clear cut band of mylonite that can be followed locally for greater than several hundred meters. The mylonitized tonalite shows lower amphibolite to upper greenschist facies metamorphism, which may indicate why there is no local uninterrupted band of mylonitization, as it metamorphosed at the brittle/ductile transition. Dated at ~92MA, it is surmised that deformation ended no later than 65-70MA due to 40Ar/40K dates from biotite in the mylonitized tonalite. Felsic pegmatite dikes also cut through the area, showing evidence of ductile shear in some places, but again, not consistently throughout the region.

Detailed mapping of the area shows a synformal structure of tonalitic mylonite between undeformed tonalite. Foliations are roughly perpendicular to the hinge line of the synform. This evidence, along with intermittent mylonitization, indicates non-uniform deformation. No evidence of overprinting was seen in the synform, suggesting that the fold formed after the majority of ductile deformation.