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Reflection Seismic Data over the La Bajada Fault zone, New Mexico, USA. Mark Hamilton SAGE 2004. Outline. Introduction & reason for obtaining a velocity model How to obtain a velocity model The results of both models The interpretation of the final stacked reflection model.
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Reflection Seismic Data over the La Bajada Fault zone, New Mexico, USA Mark Hamilton SAGE 2004
Outline • Introduction & reason for obtaining a velocity model • How to obtain a velocity model • The results of both models • The interpretation of the final stacked reflection model
CMP stack with velocity model derived from constant velocity stacks
Conclusions • Constant velocity stack model and refraction velocity model produced similar results • Surface position of fault is approximately at location 180 (~400 m from start of line) • Approximate throw of fault is 220m • Water table is at ~94m depth