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- E-ISSN: 1365-2478
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LAUFZEITANOMALIEN IM BEREICH EINER STöRUNG*
- Source: Geophysical Prospecting, Volume 1, Issue 4, Jan 1953, p. 272 - 278
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- 27 Apr 2006
Abstract
Abstract
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.