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LAUFZEITANOMALIEN IM BEREICH EINER STöRUNG *
Author(s) -
RÜHMKORF HANS ALBERT
Publication year - 1953
Publication title -
geophysical prospecting
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.735
H-Index - 79
eISSN - 1365-2478
pISSN - 0016-8025
DOI - 10.1111/j.1365-2478.1953.tb01147.x
Subject(s) - geology , tectonics , seismology , disturbance (geology) , reflection (computer programming) , cementation (geology) , economic geology , diffraction , mineralogy , telmatology , geomorphology , geophysics , optics , physics , materials science , cement , computer science , metallurgy , programming language
A bstract 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.