PASSIVE AND ACTIVE BEHAVIOR OF DOMINANT THRUST SHEETS DURING TAPER ENHANCEMENT IN THE HINTERLAND OF A FOLD-THRUST BELT WEDGE
In the Lewis segment the sedimentary basin had large initial taper (~9 degrees). Initial emplacement of the Lewis sheet required very little internal deformation of the sheet to achieve critical taper. Rocks close to the thrust were transported up from the quasi-plastic (QP) regime, and, after erosion, reached the elastico-frictional (EF) regime. Subsequent taper enhancement in the back of the wedge was accomplished by subthrust duplexing in weaker rocks that uplifted and/or transported the passive Lewis sheet. In the central Utah segment, by contrast, the initial taper of the sedimentary basin was significantly lower (~6 degrees). Initial emplacement of the dominant Canyon Range and Pavant sheets required significantly more internal deformation which was accomplished by quasi-plastic mechanisms in the lower part of the sheet. After erosion removed a significant portion of the overburden, subsequent taper enhancement of the wedge was accomplished by active deformation of the dominant internal sheets and their footwalls in the elastico-frictional (EF) regime. The contrasting styles of deformation of the dominant sheet(s) in the two examples result in two end-case scenarios of wedge evolution.