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seismic data are usually recorded over an irregular surface, and static correction has long been a problem. There are two kinds of statics, long-wavelength (large time shift) and short-wavelength (small time shift) statics.
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Seismic reflection is used to delineate the geometry of water/sediment/rock interfaces, but depending on the quality of the
data (e.g. S/N ratio), you can do amplitude-driven analysis to further investigate the nature of those interfaces. Geophysical software applications, geoservices for
near surface applications, training, consulting, tutoring. Best Tool. SmartSeis. Best Practices. Click here for a series of videos showing how to conduct a
seismic refraction survey.; Further Reading.
Seismic Refraction Exploration for Engineering Site Investigations; A Vertical Array Method for Shallow
Seismic Refraction Surveying of the Sea Floor Processing near-surface seismic-reflection data kf8 download
Reflection seismology (or
seismic reflection) is a method of exploration geophysics that uses the principles of seismology to estimate the properties of the Earth's subsurface from reflected seismic waves.The method requires a controlled seismic source of energy, such as dynamite or Tovex blast, a specialized air gun or a seismic vibrator, commonly known by the trademark name Vibroseis. BEST Processing near-surface seismic-reflection data PDF
Near-surface geophysics is the use of geophysical methods to investigate small-scale features in the shallow (tens of meters) subsurface. It is closely related to applied geophysics or exploration geophysics.Methods used include seismic refraction and reflection, gravity, magnetic, electric, and electromagnetic methods.Many of these methods were developed for oil and mineral exploration but ...
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