The spatial extent of the Deep Western Boundary Current into the Bounty Trough: new evidence from parasound sub-bottom profiling-Reference-Cited by-同舟云学术

The spatial extent of the Deep Western Boundary Current into the Bounty Trough: new evidence from parasound sub-bottom profiling

Published:2016-04-02 Issue:2 Volume:37 Page:145-158
ISSN:0025-3235
Container-title:Marine Geophysical Research
language:en
Short-container-title:Mar Geophys Res

Author:

Horn Michael,Uenzelmann-Neben Gabriele

Funder

Bundesministerium für Bildung und Forschung

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Oceanography

Link

http://link.springer.com/content/pdf/10.1007/s11001-016-9268-1.pdf

Reference44 articles.

1. Atlas Hydrographic GmbH (2010) ATLAS PARASOUND Deep-Sea parametric sub-bottom profiler. http://www.atlas-elektronik.com/what-we-do/hydrographic-systems/parasound/ , Bremen

2. Carter L, Carter RM (1988) Late quaternary development of left-bank-dominant levees in the Bounty Trough. N Z Mar Geol 78:185–197. doi: 10.1016/0025-3227(88)90108-9

3. Sedimentary Basins of the World;L Carter,1993

4. Carter RM, Carter L (1996) The abyssal Bounty Fan and lower Bounty Channel: evolution of a rifted-margin sedimentary system. Mar Geol 130:181–202. doi: 10.1016/0025-3227(95)00139-5

5. Carter L, McCave IN (1997) The sedimentary regime beneath the Deep Western Boundary Current inflow to the Southwest Pacific Ocean. J Sediment Res 67:1005–1017. doi: 10.1306/d42686b2-2b26-11d7-8648000102c1865d

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3. 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;Marine Geophysical Research;2016-10-18