The key of seismic data processing mainly lies in static corrections and imaging and both of them are relative to velocity model in complex near-surface and underground geologic structural conditions.
在复杂地表条件和复杂地质构造条件下，地震资料处理的关键主要表现为静校正和成像，而这两者均与速度模型有关。
The results of 3D seismic data processing, compared with known geologic data, showing that the C1 coherence algorithm is very effective for fault interpretation.
通过对实际三维地震资料的处理，结合已知地质资料，证明C1相干技术在三维地震资料的断层解释方面有着明显的效果。
Methods for picking out false formation boundary, and logging data processing for automatic geologic zonation are analyzed.
在此基础上，设计了测井自动地质分层算法。
Methods for picking out false formation boundary, and logging data processing for automatic geologic zonation are analyzed.
在此基础上，设计了测井自动地质分层算法。
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