Laufzeitanomalien im Bereich einer Störung
Hans Albert Rühmkorf
Journal name: Geophysical Prospecting
Issue: Vol 1, No 4, December 1953 pp. 272 - 278
Info: Article, PDF ( 379.33Kb )
The measurement of well velocity data in the well of Scheibenhardt I has shown that it is possible to observe a well noticeable measurable increase of the travel time of seismic waves when approaching a disturbance. The tectonic event of the disturbance is combined in this case with a disorder (shattering) of the layers without subsequent cementation.
The significance of these anomalies for reflection seismics is discussed. When existing they will then overlap the diffraction, treated by Th. Krey.