Comment on: “The spatial extent of the Deep Western Boundary Current into the Bounty Trough: new evidence from parasound sub-bottom profiling” by Horn and Uenzelmann-Neben-Reference-Cited by-同舟云学术

Comment on: “The spatial extent of the Deep Western Boundary Current into the Bounty Trough: new evidence from parasound sub-bottom profiling” by Horn and Uenzelmann-Neben

Published:2016-10-18 Issue:4 Volume:37 Page:371-374
ISSN:0025-3235
Container-title:Marine Geophysical Research
language:en
Short-container-title:Mar Geophys Res

Author:

Mitchell Neil C.^ORCID

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Oceanography

Link

http://link.springer.com/content/pdf/10.1007/s11001-016-9287-y.pdf

Reference13 articles.

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2. Hamilton EL (1980) Geoacoustic modeling of the sea floor. J Acoust Soc Am 68(5):1313–1340

3. Horn M, Uenzelmann-Neben G (2016) The spatial extent of the Deep Western Boundary Current into the Bounty Trough: new evidence from parasound sub-bottom profiling. Mar Geophys Res 37:145–158

4. Mayer L (1979) The origin of fine scale acoustic stratigraphy in deep-sea carbonates. J Geophys Res 84:6177–6184

5. Mayer LA (1980) Deep-sea carbonates: physical property relationships and the origin of high-frequency acoustic reflectors. Mar Geol 38:165–183

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