Tri tipa èrozionnyh formLUZGIN, B.N.Geomorfologiâ (Moskva). 2007, Num 3, pp 13-21, issn 0435-4281, 9 p.Article

Revised interpretation of tectonic features in the southern Weddell Sea, Antarctica, from new seismic dataMILLER, M; DE BATIST, M; JOKAT, W et al.Polarforschung. 1990, Vol 60, Num 1, pp 33-38, issn 0032-2490Article

Impact of the continental shelf slope on upwelling through submarine canyonsHOWATT, T. M; ALLEN, S. E.Journal of geophysical research. Oceans (Print). 2013, Vol 118, Num 10, pp 5814-5828, issn 2169-9275, 15 p.Article

WIND EFFECTS ON CURRENTS OBSERVED IN JUAN DE FUCA SUBMARINE CANYONCANNON GA.1972; J. PHYS. OCEANOGR.; U.S.A.; DA. 1972; VOL. 2; NO 3; PP. 281-285; BIBL. 13 REF.Serial Issue

Geospatial variability of krill and top predators within an Antarctic submarine canyon systemSANTORA, Jarrod A; REISS, Christian S.Marine biology (Berlin). 2011, Vol 158, Num 11, pp 2527-2540, issn 0025-3162, 14 p.Article

Les réseaux de paléovallées et de canyons des approches occidentales de la Manche = The networks of paleovalleys and canyons from the Channel Western ApproachesBOURILLET, J. F; PEYRE, S; HENRIET, J. P et al.Réunion des Sciences de la Terre. 1998, p. 81Conference Paper

Un canyon sous-marin revisité : le trou sans fond de Côte d'IvoireVANNEY, J. R; MASCLE, J.Annales de géographie (Paris). 1992, Vol 101, Num 563, pp 43-67, issn 0003-4010Article

Geomorfologija Ohotomorskogo sklona o-va Iturup (Bol'šaja Kuril'skaja grjada)VOL'NEV, V. M; GLADYŠEV, I. N.Geomorfologiâ (Moskva). 1990, Num 4, pp 57-63, issn 0435-4281Article

Novye dannye o rel'efe dna i otloženiâh na šel'fe i kontinental'nom sklone zapadnoj časti Čërnogo morâ, polučennye v zapisâh èholotnogo promeraEVSÛKOV, Û.D.Geomorfologiâ (Moskva). 2007, Num 1, pp 51-63, issn 0435-4281, 13 p.Article

Sediment-driven downslope flow in submarine canyons and channels : Three-dimensional numerical experimentsKÄMPF, Jochen; FOHRMANN, Hermann.Journal of physical oceanography. 2000, Vol 30, Num 9, pp 2302-2319, issn 0022-3670Article

Main observations on genesis and morphological evolution of submarine valleysDE PIPPO, T; ILARDI, M; PENNETTA, M et al.Zeitschrift für Geomorphologie. 1999, Vol 43, Num 1, pp 91-111, issn 0372-8854, 21 p.Article

The response of a steep-sided, narrow canyon to time-variable wind forcingHICKEY, B. M.Journal of physical oceanography. 1997, Vol 27, Num 5, pp 697-726, issn 0022-3670Article

Rel'ef central'noj časti Dunajskogo konusa vynosaEVSJUKOV, Ju. D; KARA, V. I.Geomorfologiâ (Moskva). 1990, Num 2, pp 71-75, issn 0435-4281Article

Morfologiâ podvodnyh kan'onov Zapadno-Kavkazskogo rajona Černogo morâBLINKOVA, O.A.Geomorfologiâ (Moskva). 2001, Num 4, pp 51-58, issn 0435-4281, 8 p.Article

EVOLUTION OF VEATCH, WASHINGTON, AND NORFOLK SUBMARINE CANYONS; INFERENCES FROM STRATA AND MORPHOLOGY = EVOLUTION DES CANYONS SOUS-MARINS DE VEATCH, WASHINGTON ET NORFOLK: INFERENCES D'APRES LES STRATES ET LA MORPHOLOGIEFORDE EVAN B.1981; MAR. GEOL.; ISSN 0025-3227; USA; DA. 1981-02; VOL. 39; NO 3-4; PP. 197-214; BIBL. 26 REF.; ILL.Article

Temporal evolution of lead isotope ratios in sediments of the Central Portuguese Margin: A fingerprint of human activitiesMIL-HOMENS, Mário; CAETANO, Miguel; COSTA, Ana M et al.Marine pollution bulletin. 2013, Vol 74, Num 1, pp 274-284, issn 0025-326X, 11 p.Article

Muscular and Hepatic Pollution Biomarkers in the Fishes Phycis blennoides and Micromesistius poutassou and the Crustacean Aristeus antennatus in the Blanes Submarine Canyon (NW Mediterranean)SOLE, Montserrat; HAMBACH, Bastian; CORTIJO, Verónica et al.Archives of environmental contamination and toxicology (Print). 2009, Vol 57, Num 1, pp 123-132, issn 0090-4341, 10 p.Article

Assemblages in a submarine canyon : influence of depth and timeSABATINI, A; FOLLESA, M. C; LOCCI, I et al.Hydrobiologia (The Hague). 2007, Vol 580, pp 265-271, issn 0018-8158, 7 p.Conference Paper

In-situ measurements of velocity structure within turbidity currentsXU, J. P; NOBLE, M. A; ROSENFELD, L. K et al.Geophysical research letters. 2004, Vol 31, Num 9, pp L09311.1-L09311.4, issn 0094-8276Article

Transport of persistent organic pollutants by organo-mineral aggregates (OMAs) in the Lisboa-Setúbal Canyon systemDE JESUS MENDES, Pedro A; THOMSEN, Laurenz; GARCIA, Rosa et al.Deep-sea research. Part 2. Topical studies in oceanography. 2011, Vol 58, Num 23-24, pp 2345-2353, issn 0967-0645, 9 p.Article

The effects of boundary turbulence on canyon flows forced by periodic along-shelf currentsBOYER, Don L; SOMMERIA, Joel; MITROVIC, Andjelka Srdic et al.Journal of physical oceanography. 2006, Vol 36, Num 5, pp 813-826, issn 0022-3670, 14 p.Article

Gradients in activity and biomass of the small benthic biota along a channel system in the deep Western Greenland SeaSOLTWEDEL, Thomas; HASEMANN, Christiane; QUERIC, Nadia-Valérie et al.Deep-sea research. Part 1. Oceanographic research papers. 2005, Vol 52, Num 5, pp 815-835, issn 0967-0637, 21 p.Article

Faciés acoustiques du système turbiditique recent du Zaïre (projet Zaiango) = Acoustical facies of the recent turbiditic system from Zaire (Zaiango project)CREMER, M; SAVOYE, B.ASF Association des sédimentologistes français. 1999, pp 93-94, issn 0990-3925, isbn 2-907205-32-3Conference Paper

SWAN predictions of waves observed in shallow water onshore of complex bathymetryGORRELL, L; RAUBENHEIMER, B; ELGAR, Steve et al.Coastal engineering. 2011, Vol 58, Num 6, pp 510-516, issn 0378-3839, 7 p.Article

Distribution of suspended sediment in the coastal sea off the Ganges-Brahmaputra River mouth: observation from TM dataMOHAMMAD REZWANUL ISLAM; SYEDA FAHLIZA BEGUM; YAMAGUCHI, Yasushi et al.Journal of marine systems. 2002, Vol 32, Num 4, pp 307-321, issn 0924-7963Article