A bstract A process is described whereby the interpretation of seismic reflection data is carried out by a preliminary two‐dimensional plotting procedure followed by a three‐dimensional migration. The concept of a surface of maximum convexity is introduced as an integral part of the process of migration. The procedures for deriving the necessary charts of curves are considered and a number of serviceable charts presented.
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J. G. Hagedoorn (1954) studied this question.
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