We discuss travel-time anomalies produced by near-surface low velocity weathered zones and variable topographic relief. These features produce travel-time anomalies often referred to as static anomalies because the delays are common to all deeper events viewed through this near surface lens.
- Күн бұрын
Geophysics - Seismic: Static anomalies in reflection seismic data
- Рет қаралды 1,630
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