1887
Volume 22 Number 3
  • E-ISSN: 1365-2478

Abstract

A

A correct derivation of rms, average and interval velocities from one another and from common depth point stacking velocities requires a clear understanding of the relationships between these velocities. We relate the average velocity to the rms velocity through a “heterogeneity factor” which is a quantity that gives a measure of the degree of velocity heterogeneity in the ground. The interval velocity is a quantity which varies according to the method of its derivation. The difference between rms and stacking velocities depends on the heterogeneity factor and on the length of the spread. Unless allowed for, this difference can reverse the advantages of long spreads and cause large errors in interval velocity determinations. It may be removed through a number of techniques. The accuracy of stacking velocities in the presence of random “noise” is independent of the heterogeneity factor. Relevant expressions can be broken down into simple formulae which give the accuracy quickly and with good precision.

Loading

Article metrics loading...

/content/journals/10.1111/j.1365-2478.1974.tb00099.x
2006-04-27
2024-04-26
Loading full text...

Full text loading...

References

  1. Al‐Chalabi, M., 1973, Series approximation in velocity and traveltime computation. Geophysical Prospecting21, 783–795.
    [Google Scholar]
  2. Bodoky, T., and Szeidovitz, Zs., 1972, The effect of normal correction errors on the stacking of common‐depth point traces. Geophysical Transactions of the Hungarian Geophysical Institute Roland Eötvös, 20 (3–4), 47–57.
    [Google Scholar]
  3. Brown, R. J. S., 1969, Normal‐moveout and velocity relations for flat and dipping beds and for long offsets. Geophysics34, 180–195.
    [Google Scholar]
  4. Dix, C. H., 1955, Seismic velocities from surface measurements. Geophysics20, 68–86.
    [Google Scholar]
  5. Schneider, W. A., 1971, Developments in seismic data processing and analysis (1968–1970). Geophysics36, 1043–1073.
    [Google Scholar]
  6. Taner, M. T., and Koehler, F., 1969, Velocity spectra—Digital computer derivation of velocity functions. Geophysics34, 859–881.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/journals/10.1111/j.1365-2478.1974.tb00099.x
Loading
  • Article Type: Research Article

Most Cited This Month Most Cited RSS feed

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