On the central Nile deep-sea fan, stratified sediments overlying mass-transport deposits (MTDs) are deformed into slope-parallel seabed undulations associated with fluid seepage. The western part of this system, in water depths of 1,950-2,250 m, is examined using multi-frequency data from hull-mounted and deep-towed swath/profiling systems....
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2014 (v1)Journal articleUploaded on: December 3, 2022
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2009 (v1)Journal article
Oceanography, v. 22, n. 1, p. 92-109, 2009
Uploaded on: December 4, 2022 -
2009 (v1)Journal article
Marine Geophysical Researches, v. 29, n. 4, p. 275-290, 2009. http://dx.doi.org/10.1007/s11001-009-9063-3
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2008 (v1)Journal article
Earth and Planetary Science Letters, v. 274, n. 1-2, p. 34-39, 2008. http://dx.doi.org/10.1016/j.epsl.2008.06.047
Uploaded on: December 3, 2022