An algorithm for rapid generation of (r,p) plots following the method of Kennett (1981) is implemented in FORTRAN 77. Computations proceed in the frequency domain (w,p) and are Fourier transformed to (r,p). Elastic and acoustic models for layers embedded between half spaces are used to generate (r,p) plots by means of basic calcomp plot modules. Models are presented to test the program reliability for low-velocity layers, generation of internal multiples, mode conversion, and variations in depth and type of receiver (vertical, horizontal, and pressure). A brief outline of the theory and a program listing are included.
Frazer, L. N., and Rudman, A. J., 1988, Seismic modeling in the (t,p) domain: Indiana Geological Survey Occasional Paper 54, 55 p., 10 figs., 7 tables, 4 app.
You may also like:
Can't find what you're looking for? Feel free to contact us directly:
Publication Sales Office
Indiana Geological and Water Survey
420 N. Walnut St.
Bloomington, IN 47404
IGS Return Policy
All sales are final. Materials may not be returned after they have been accepted by the customer. Any discrepencies in mail orders must be reported to IGWS within 10 days of receipt of order.
The Indiana Geological and Water Survey will refund the purchase price and sales tax of products if returned with the original sales receipt within 10 days of receipt of order. Refunds will be issued with the same method of payment as indicated on the original receipt except for cash purchases, which will be refunded by check. Items must be returned in the same condition as purchased. Refunds on digital products and services are not allowed, except for defective media such as CD-ROMs, flash drives, and so on. The customer is responsible for paying shipping costs to return items.