Chronostratigraphic Color Decomposition: A Fast Method for Identifying Sedimentary Features in Seismic Data

The temporal chromatic decomposition methodology offers an alternative interpretation workflows. By utilizing RGT properties, this approach operates in two modes: horizon-based and horizon stack. The horizon mode enhances interpretation accuracy by normalizing input offsets and minimizing artifacts from signal intersections, preserving the geological morphology of structures. The horizon stack mode enables rapid visualization of broader stratigraphic frameworks, aiding in the identification of key sedimentary and structural features with real-time flexibility.

This method ensures geologically consistent results, with colors representing depth relative to the observed attribute, allowing interpreters to extract meaningful insights efficiently. Its dual functionality accelerates seismic interpretation workflows, making it particularly valuable for detailed stratigraphic analyses of large, complex datasets. The temporal chromatic decomposition provides geoscientists with a powerful tool for improving accuracy, efficiency, and the overall quality of seismic data interpretation.