. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. 166 WORZEL AND HARRISON [chap. 9 of Cruiser Bank. Some seismic data (Bentley et al., iinpiil)lislied) exist on the seamount and in the nearby flanking regions to provide control on the upper parts of the sections. A two-dimensional analysis was used to compute the variations of the M-discontinuity which would be required to accoinit for the gravity anomaly (Worzel and Talwani, 1959a). Fig. 24 shows the resulting section. Since this feature is not perfectly represented by a two-dimensional Observed grovity. Topography
. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. 166 WORZEL AND HARRISON [chap. 9 of Cruiser Bank. Some seismic data (Bentley et al., iinpiil)lislied) exist on the seamount and in the nearby flanking regions to provide control on the upper parts of the sections. A two-dimensional analysis was used to compute the variations of the M-discontinuity which would be required to accoinit for the gravity anomaly (Worzel and Talwani, 1959a). Fig. 24 shows the resulting section. Since this feature is not perfectly represented by a two-dimensional Observed grovity. Topography ;' ^ km/sec; ' ; '. 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 Hill, M. N. (Maurice Neville), 1919-. New York : Interscience Pub.
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Keywords: ., bookcentury1900, bookcollectionbiodivers, booksubjectoceanbottom
