1887

Abstract

The paper proposes an effective method to recover a thin-formation structure (thinner than seismic wavelength) through amplitude inversion of surface-recorded low-frequency seismic events with due regard for downhole acoustic log data. As a result, spatial structure and properties of individual thin beds in a geologic unit are recovered between the wells at a scale less than seismic wavelength.

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/content/papers/10.3997/2214-4609-pdb.20.A026
2006-10-16
2020-09-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.20.A026
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