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Definition


Scanning for acoustic properties of rocks along a certain straight line on the surface by generating a low frequency noise at central point of the line and capturing the acoustic response in array set of sensors along the selected survey line (see Fig. 1).

Two Way Time Illustration

Fig.1. Seismic reflection schematic


The result of the survey is pictured as vertical profile (see Fig. 2) with:

  • Horizontal axis showing a distance along the seismic line

  • Vertical axis showing

    • either a TWT travel time of acoustic wave towards the seismic reflection boundary at normal-incidence

    • or a depth at which the seismic reflection boundary is found (which is related to travel time via p-wave velocity)

  • Colour is showing the Reflection Coefficient at inter-bed boundary

Image result for seismic profile

Fig. 2. Sample of seismic reflection profile in TWT format.



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