Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6433995 | Tectonophysics | 2013 | 13 Pages |
â¢3-D coverage of crust and mantle in S. Ontario via complementary imaging methodsâ¢Detection of layered crust with breaks corresponding to major structural featuresâ¢Ottawa-Bonnechère Graben is a crustal-scale feature that offsets the Moho.â¢Mississauga Domain is bounded by crustal-scale faults.â¢Upper mantle contains dipping features possibly related to subduction remnants.
A teleseismic data set from the POLARIS project is used to obtain 3-D images of southern Ontario using two imaging techniques: scattering tomography and common-conversion-point stacking. The resulting images reveal a layered crust, the layering being interrupted by discontinuities associated with major crustal-scale faulting. Breaks in crustal continuity and Moho deflections associated with the Ottawa-Bonnechère Graben indicate that the graben is associated with faulting on a whole crust scale. We also detect similar discontinuities across the Mississauga Domain, supporting the previous interpretation that the domain is bounded by crustal-scale faults. We locate discontinuous sub-lithospheric negative-polarity arrivals which indicate complex three-dimensional structures within the lithosphere and may be associated with subduction remnants or a mid-lithosphere discontinuity.