Results of a Deep-Tow Multichannel Survey on the Bermuda Rise
1988
Gettrust, J. F. | Grimm, M. | Madosik, S. | Rowe, M.
High-resolution multichannel seismic data taken with a deep-towed source and receiving array are used to obtain estimates of the in situ compressional velocity-depth functions within the upper approx. 300 m of deep- ocean sediments. These data, taken on the Bermuda Rise in an area with a nominal water depth of 5 km, resolve structure consistent with DSDP data from the region. The velocity-depth functions derived from these data indicate little P- velocity gradient in the upper 100-170 m of sediments and resolve P-velocity inversions within the depth range sampled. Keywords : Ocean bottom sediments; Seismic data. Reprints.
Show more [+] Less [-]Pub. in Geophysical Research Letters, v15 n12 p1413-1416 Nov 1988.
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