. Computer programs in oceanography. Oceanography. 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
. Computer programs in oceanography. Oceanography. 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- SACKIN AND SNEATH, UNlV. OF LEICESTER. 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-DIM
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Keywords: ., bookcentury1900, bookcollectionbiodiver, booksubjectoceanography
