Abstract

In regions where reflections can be correlated from point to point the mapping of faults presents little difficulty, and the hade as well as the throw of a fault can be generally determined. Two records secured across a fault are reproduced and a cross section derived from these records is shown. A description is given of a method of profiling which permits correlation of records in areas where the ordinary correlation method cannot be successfully applied. The application of this method in the determination of faults is outlined.

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