1887
Volume 1 Number 4
  • E-ISSN: 1365-2478

Abstract

A

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.

Loading

Article metrics loading...

/content/journals/10.1111/j.1365-2478.1953.tb01147.x
2006-04-27
2020-10-31
Loading full text...

Full text loading...

References

  1. H.Reich, Erdöl und Kohle4 (1951), S.. 538.
    [Google Scholar]
  2. Th, Krey, Mündliche Mitteilung.
    [Google Scholar]
  3. TH, KREY, Geophysics, XVII (1952), S. 843.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/journals/10.1111/j.1365-2478.1953.tb01147.x
Loading
  • Article Type: Research Article
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error