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Abstract

Summary

This paper considers results of upper section velocity model creation using first arrivals tomography and Full Waveform Inversion of Early-Arrival Waveform. The comparison is made for different models and the limitations and advantages of each method in specific geological conditions are shown. Reliable solution for creating near-surface model is premised not only on using well- known and proven seismic algorithms such as Generalized Linear Inversion (GLI3D) or Early-Arrival Waveform Tomography (FWI). It also includes joint inversion of electrometry and microgravimetry data. The solution obtained for near-surface velocity model satisfies not only the measured seismic, but also electrical and gravitational fields.

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/content/papers/10.3997/2214-4609.202051153
2020-09-14
2024-04-28
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References

  1. DanielR.H. O’Connell, Weizhong Wang, JieZhang
    , 2011, 3D joint inversion of seismic traveltime and gravity data: a case study Dengguo Zhou*1, 81st Annual International Meeting, SEG, Expended Abstracts, 30, 3148–3152.
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