FIELD: seismic prospecting. SUBSTANCE: elastic vibrations are excited by vibration sources working for two sessions. During first session elastic vibrations with initial frequency ωн and final frequency ωx are excited starting from frequency ωн up to upper boundary frequency ωsb of spectrum of transverse waves. Seismic vibrations are received by groups of horizontal geophones and beginning from lower boundary frequency ωpн of spectrum of transverse waves up to frequency ωx by groups of vertical geophones. During second session elastic vibrations are generated within frequency range from ωpн to ωsb and components of seismic vibrations with polarity of one of them changed for reverse one are simultaneously received by horizontal and vertical geophones. In this case pulse seismograms are reconstructed after operation of addition-subtraction for transverse waves in frequency range from ωн to ωsb and for longitudinal waves in frequency range from ωpн to ωx. EFFECT: enhanced authenticity of results of seismic prospecting. 3 dwg
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Authors
Dates
1995-10-27—Published
1990-07-23—Filed