Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9536209 | Journal of Structural Geology | 2005 | 19 Pages |
Abstract
The sense of shear may be constant across an HGNA shear zone, giving it the geometry and kinematics of a crustal-scale (kilometres thick) detachment zone. Alternatively it may reverse across the body, consistent with channel flow. Structural evidence therefore supports current ideas on the behaviour of the middle to lower crust during orogeny, and illustrates the deformation mechanisms involved. We describe the association with special reference to the Monashee complex, and discuss the implications of our interpretation for the kinematics of high-strain zones, palinspastic reconstruction, and interpretation of deformation fabrics at various scales.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Paul F. Williams, Dazhi Jiang,