The quality of horizon tracking is one of the key challenges in seismic interpretation.
It is also one of the most time-consuming tasks.
Nowadays there is a large number of auto tracking algorithms available. However, addressing a structural interpretation workflow in a complex geological environment still poses considerable technological limitations. This drive both project timings and costs up.
Accurate salt body interpretation (and other similar stratigraphic objects) usually presents a complex challenge for geoscientists. Extreme dip values, doubtful horizon interpretation (including multi-Z cases), velocity anomalies and poor reflectivity data - all these factors contribute to uncertainties in interpretation.
Traditional multi-attribute analysis techniques combined with RGB blending (or other blending variations) allow to identify geological objects in the seismic volume with a reasonable degree of accuracy. However, this approach has major disadvantages, such as false probabilities and the need to run complex and often
time-consuming attribute calculations.