{"refrec":{"BRefID":240764,"RR":"<b>Kelling, G.; Stanley, D.J.</b> (1972). Sedimentary evidence of bottom current activity, Strait of Gibraltar region. <i>Mar. Geol. 13(3)</i>: 51-60. <a href=\"http://dx.doi.org/10.1016/0025-3227(72)90087-4\" target=\"_blank\">http://dx.doi.org/10.1016/0025-3227(72)90087-4</a>","BEntID":232461,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Mar. Geol. 13(3)</i>: 51-60. <a href=\"http://dx.doi.org/10.1016/0025-3227(72)90087-4\" target=\"_blank\">http://dx.doi.org/10.1016/0025-3227(72)90087-4</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Kelling, G.; Stanley, D.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Kelling, G.; Stanley, D.J.","Englishabstract":"Orientated photographs of the sea-bed, together with grab and short-core sediment samples, at 18 stations in the Strait of Gibraltar region confirm the presence in the Strait of powerful and persistent westward-directed bottom currents. Sedimentary structures and textures provide data on the direction and strength of this bottom flow which are consistent with existing hydrologic observations of the Mediterranean undercurrent. 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