De. Boerner et al., Seismic images and three-dimensional architecture of a Proterozoic shear zone in the Sudbury Structure (Superior Province, Canada), TECTONICS, 19(2), 2000, pp. 397-405
A broad zone of intense ductile to brittle deformation transects the Paleo-
Proterozoic Sudbury Igneous Complex and likely formed during the final stag
es of the Penokean orogeny on the southern margin of the Superior Province.
Herein we present a three-dimensional image of this deformation zone, deri
ved from four seismic reflection profiles. Additional information from rock
property measurements, drill results, and published structural mapping sug
gests that the seismic data define the three-dimensional disposition of lis
tric shear zones. The seismic image of the deformation is best developed wi
thin the Onaping Formation. However, the images of the deformation zone env
elope are imperfect, being most clear where truncating known contacts withi
n the Sudbury Igneous Complex and its contact with Huronian host rocks. The
southern edge of the seismically imaged shear zones does not extend signif
icantly beyond the exposed Sudbury Igneous Complex, suggesting limits to th
e extent of deformation in the Sudbury Structure.