Seismic data are usually processed to be zero-phase, and we usually assume that the phase is stable in space and time. Indeed, these assumptions are central to most AVO and other quantitative work.
There are four simple ways to help determine phase:
- Well ties
- Instantaneous phase
- Rotation tests
In general, you are unlikely to be able to see a phase difference of 15° or less, and indeed it probably would not matter for horizon picking or even quantitative work. A phase rotation of 30° is probably worth fixing for quantitative work. anything more than 45° is worth fixing even for interpretation.
Beware: undoing the picking you do on a phase rotated volume is onerous: only make a rotation of your data when you are sure it is more geological that way.
Simply examining a strong seismic event that corresponds to an isolated geologic surface of known impedance contrast. It helps if the contrast, which must be spatially consistent in polarity, is fairly strong. Good examples are the seafloor, the Wabamun (in Western Canada), and the Devonian Unconformity (in the Athabasca oil sands).
A good workflow is to tie wells with a zero-phase wavelet, at least at first. Wehn tying, make a note of the phase disparity at the well — many software tools let you plot correlation coefficient against phase rotation. Once you have a feel for the variance of the well ties, you can start to see if there are spatial trends in this variance. Perhaps most wells tie better with a 90° phase rotation.