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Reading Waves. Using Seismic D ata. Vibroseis units similar to this are common as sources in land reflection seismic surveys – They substitute for explosives –several are used together - radio controlled and synchronized. Refracted Wave. Waves used in reflection seismology.

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Reading waves

Reading Waves

Using Seismic Data


  • Vibroseis units similar to this are common as sources in land reflection seismic surveys – They substitute for explosives –several are used together - radio controlled and synchronized





Equations for finding the thickness of the layers
Equations for finding the thickness of the layers velocity of the direct wave.

  • ic0 - critical angleV0 - velocity of the first layerV1 - velocity of the second layerh0 - thickness of the first layerT01 - intercept


Waves used in reflection seismology1
Waves used in reflection seismology velocity of the direct wave.


Sample data from the workshop
Sample Data from velocity of the direct wave.the Workshop


Cropped data
Cropped Data velocity of the direct wave.


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