ERANCE (DELTA) THOSE POINTS X(I) ALONG A GIVEN CLOSED INTERVAL FOR 

 WHICH THE FUNCTIONAL VALUE FX(I) SATISFIES THE ABSOLUTE VALUE OF FX(I) 

 LESS THAN DELTA. EACH POINT AND THE CORRESPONDING FUNCTIONAL VALUE 

 ARE STORED IN A TABLE. NRL MEMO. REPORT 197^. AUTHORS — J. MASON. 

 H. TOOTHMAN. 



JANET P. MASON 



RESEARCH COMPUTATION CENTER 



MATHEMATICS AND INFORMATION SCIENCES DIVISION 



NAVAL RESEARCH LABORATORY. WASHINGTON, D. C. 20390 



CROSS-ASSOCIATION OF NONNUMERIC SEQUENCES LANGUAGE - ALGOL 60 AND 



FORTRAN IV 

 COMPUTER - ELLIOTT 803C 

 IBM 7040/^4 



READS A PAIR OF SEQUENCES WHOSE ELEMENTS BELONG TO A NONORDERED SET. 

 THE DATA ARE READ IN A NUMERIC CODE. THE PROGRAM SLIDES THE SEQUENCES 

 PAST EACH OTHER ONE OR MORE STEPS AT A TIME AND FOR EACH MATCH POSI- 

 TION COUNTS THE NUMBER OF COMPARISONS (SIZE OF OVERLAP). VARIOUS SIG- 

 NIFICANCE MEASURES AND OVERALL SIMILARITY ESTIMATES ARE MADE. AUTHORS- 

 M.J. SACKIN AND P.H.A. SNEATH, UNlV. OF LEICESTER. D.F. MERRIAM, KAN- 

 SAS GEOL. SURVEY. REF. SPECIAL DISTRIbUTION PUBLICATION 23 (1965). 



DR. DANIEL F. MERRIAM, EDITOR, COMPUTER CONTRIBUTIONS 

 KANSAS GEOLOGICAL SURVEY 

 COMPUTER APPLICATIONS LABORATORY 

 THE UNIVERSITY OF KANSAS 

 LAWRENCE. KANSAS 660^5 



SIMULATION OF TRANSGRESSION AND REGRESSION WITH LANGUAGE - FORTRAN IV 

 CONTINUOUS-TIME MARKOV MODELS COMPUTER - CDC 6400 



REPORT (COMPUTER CONTRIBUTION 26) IS CONCERNED WITH A STOCHASTIC SIMU- 

 LATION MODEL IN WHICH THE PATTERN OF LITHOLOGIC SUCCESSION IS EXAMINED 

 IN TERMS OF THE LENGTH OF TIME THAT THE SYSTEM REMAINS IN A GIVEN 

 STATE, ONCE IT HAS ENTERED THAT STATE. THE MODEL IS ALSO BAsEd ON 

 TRANSGRESSIVE-REGRESSIVE MOTION OF A SHORELINE (OR STRANDlINE), W 

 THE RESULTING LITHOLOGIC UNITS DEVELOPING AS RESPONSES TO THE MOV 



ITH 

 MOVEMENT 



DR. DANIEL F. MERRIAM, EDITOR 

 COMPUTER CONTRIBUTIONS 

 KANSAS GEOLOGICAL SURVEY 

 THE UNIVERSITY OF KANSAS 

 LAWRENCE, KANSAS 6604'^ 



POWER SPECTRUM OF GEOLOGICAL SURFACES LANGUAGE - FORTRAN IV 



COMPUTER - GE 625 AND 

 IBM 7040 



TWO-DIMENSIONAL POWER SPECTRUM IS USED FOR NUMERICAL DESCRIPTION OF 

 OBSERVED SURFACES. DATA MUST BE GRIDDED - MAXIMUM IS 100 BY lOO 

 POINTS. RUNNING TIME FOR MAXIMUM ARRAY IS ABOUT 20 MINUTES ON GE 625. 

 COMPUTER CONTRIBUTION 16. BY J.E. ESLER AND F.W. PRESTON. 1967. 



DR. DANIEL F. MERRIAM. EDITOR 

 COMPUTER CONTRIBUTIONS 

 KANSAS GEOLOGICAL SURVEY 

 THE UNIVERSITY OF KANSAS 

 LAWRENCE. KANSAS 66044 



PAGE 054 



