Methodological tutorial demonstrates enhanced deepwater channel architectural mapping via dual-attribute corendering, highlighting improved reservoir interpretation confidence in frontier exploration.
Seismic interpretation of deepwater channel systems requires delineation of architectural elements (AEs) whose acoustic impedance contrasts are often subtle and whose amplitude responses can be non-unique. Standard amplitude displays conflate reflector geometry with lithologic properties, complicating facies predictions and architectural boundary mapping. This tutorial demonstrates a systematic corendering technique using two widely available attributes: cosine of instantaneous phase (cosφ) and relative acoustic impedance (RAI). These attributes address amplitude interpretation limitations by separating complimentary tasks: cos? provides amplitude-independent mapping of reflector terminations and (dis)continuous reflector patterns that define channel stratigraphy, whereas RAI enables property-based characterization of lateral and vertical facies variations. We present a five-step optimization workflow (attribute extraction, corendering methodology, colormap selection, sampling rate adjustments, and spectral balancing) applied to a deepwater channel complex in New Zealand’s Taranaki Basin. Results demonstrate significant improvement in architectural element visibility compared to conventional amplitude interpretation, enabling confident identification of erosion surfaces, channel stacking patterns, and stratigraphic terminations. This optimized visualization approach provides the foundation for systematic interpretation workflows applicable to exploration settings where limited well control and complexity of deepwater channel settings require transparent evaluation of interpretation confidence.
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Moreno-Ward et al. (2026) studied this question.
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