Date post: | 03-Jan-2016 |
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High P and T Experiments
Density, Gravity, Pressure and Mass Distributions
Temperature in the Earth
Attenuation
FrequencyLow High
Ene
rgy
radiated signal
attenuated signal
lost energy
peak
peak
Exploration seismology
• Determine the seismic velocity structure in the shallow part of the Earth, using active sources.
• Procedures: Acquisition, Processing and Interpretation.
Gather
Velocity Analysis
NMO Corrections
Mute
Statics Corrections
Stack
Migrations