Depth-focusing analysis (DFA), a method of refining velocities for pre
stack depth migration, relies on amplitude buildups at zero offset to
determine the extrapolation depths that best focus the migrated data.
Unfortunately, seismic energy from dipping interfaces, diffractions, a
nd noise often produce spurious amplitude indications of focusing. To
reduce possible ambiguity in the DFA interpretation process, we introd
uce a new attribute for determining focusing that is relatively indepe
ndent of amplitude. Our approach is based on estimates of the radius o
f wavefront curvature. The estimates are derived from normal moveout a
nalysis of nonzero-offset data saved during migration. By relating ste
eper moveout to smaller radius of wavefront curvature, focusing is def
ined by a wavefront curvature of zero radius. Additionally, we show th
at applying inverse-radius weights to the amplitude data attenuates no
nfocused events due to their large radius of curvature. Using the Marm
ousi data set, our weighting scheme resulted in reduced spurious focus
ing and enhanced velocity resolution in DFA.