. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. 105, 10- 10- 2 10" "^^ 1- ^ z i^ 103 v s O 10' I 1— < u. UJ 10° O P. * B-B' A-A 10-3 10-2 10-' 10° NORMALIZED FREQUENCY (CYCLES/DATA INTERVAL) 10' Figure 4-10 Composite of Figures 4-8 and 4-9 Illustrating the anisot- ropy of the sea floor In the Mendocino Fracture zone. Although both spectra retain their power law form, there Is an obvious difference In slope and Intercept. Profile B-B' appears to contain more high spatial frequency energy, while profile A-A' cont
. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. 105, 10- 10- 2 10" "^^ 1- ^ z i^ 103 v s O 10' I 1— < u. UJ 10° O P. * B-B' A-A 10-3 10-2 10-' 10° NORMALIZED FREQUENCY (CYCLES/DATA INTERVAL) 10' Figure 4-10 Composite of Figures 4-8 and 4-9 Illustrating the anisot- ropy of the sea floor In the Mendocino Fracture zone. Although both spectra retain their power law form, there Is an obvious difference In slope and Intercept. Profile B-B' appears to contain more high spatial frequency energy, while profile A-A' contains more energy In lower spatial frequencies. 39. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Fox, Christopher Gene; United States. Naval Oceanographic Office. Bay St. Louis, Miss. : Naval Oceanographic Office
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Keywords: ., bookcentury1900, bookcollectionbiodivers, booksubjectoceanbottom
