LAUFZEITANOMALIEN IM BEREICH EINER STöRUNG*

1 December 1953

journal article
Published by Wiley in Geophysical Prospecting

Vol. 1 (4) , 272-278
https://doi.org/10.1111/j.1365-2478.1953.tb01147.x

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.

Keywords

EINER STORUNG
BEREICH EINER
LAUFZEITANOMALIEN IM
IM BEREICH
CEMENTATION
VELOCITY DATA
WELL VELOCITY

This publication has 1 reference indexed in Scilit:

THE SIGNIFICANCE OF DIFFRACTION IN THE INVESTIGATION OF FAULTS
Geophysics, 1952