1887

Abstract

It is common knowledge that a discontinuous increase in seismic impedance produces a<br>reflection of positive polarity and a discontinuous decrease produces a reflection of negative<br>polarity. That knowledge seldom is applied in engineering contexts, however, because the<br>polarity of seismic reflections is not always obvious. That is particularly true in the case of<br>single-channel marine data when signal amplitude is displayed on paper as shades of grey. This<br>contribution documents a case in which reflection polarity was critical not only to the<br>interpretation of the seismic data but also to the client’s profit margin.

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/content/papers/10.3997/2214-4609-pdb.203.1998_029
1998-03-22
2024-04-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.203.1998_029
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