A three component VSP experiment was carried out in the metasedimentar
y Whitewater group of the Sudbury Structure. Processing of the VSP dat
a focused on velocity analysis, wavefield separation, shear-wave analy
sis, waveform modelling, hodogram analysis, and integration of surface
-seismic and borehole geophysical data. Wavefield separation processin
g and synthetic VSP modelling resulted in a realistic velocity model a
nd the corridor-stacked compressional section correlates well with the
surface seismic reflection data. The shear wave section provides an a
dditional constraint on the subsurface structure. Besides establishing
a direct link between borehole lithologies and surface seismic images
, the VSP data, using three component particle motion velocity hodogra
ms, provide an independent estimate of true reflector dip in the subsu
rface of the Sudbury Structure.