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DEPARTMENT OF APPLIED MATHEMATICS THE WEIZMANN INSTITUTE OF SCIENCE, REHOVOT, Israel
Abstract
The use of cubic-spline functions for the smoothing of seismological travel-times data is suggested. This smoothing method is compared with other methods used for that purpose. The final stages of the production of the Herrin P-tables are critically examined, and the use of cubic-spline functions for their smoothing is shown to improve the resulting table.
Footnotes
* Permanent address: A.E.R.E., Harwell, Didcot, Berkshire, England.
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