Late Quaternary sedimentation within a submarine channel-levee system offshore Cap Timiris, Mauritania

Marine Geology

Volumn 240, Issue 1-4, 2007, Pages 217-234

  Zuhlsdorff C ^a   Wien, K ^a   Stuut, J B W ^a   Henrich, R ^a  

^a UNIVERSITY OF BREMEN   (Germany)

Author keywords

aeolian supply; continental margin; end members; Holocene; late Pleistocene; marine sediments; north west Africa; sedimentary processes

Indexed keywords

AEOLIAN SUPPLY; CONTINENTAL MARGIN; END MEMBERS; HOLOCENE; LATE PLEISTOCENE; MARINE SEDIMENTS; NORTH WEST AFRICA;

ARID REGIONS; DUST; GRAIN SIZE AND SHAPE; SEA LEVEL; SEDIMENT TRANSPORT; SEDIMENTATION;

SUBMARINE GEOLOGY;

ALLUVIAL DEPOSIT; CLIMATE CHANGE; CONTINENTAL MARGIN; EOLIAN DEPOSIT; EOLIAN PROCESS; FLUVIAL DEPOSIT; GRAIN SIZE; HOLOCENE; LEVEE; MARINE RECORD; MARINE SEDIMENT; PALEOCLIMATE; PLEISTOCENE; RECONSTRUCTION; RIVER DISCHARGE; SEDIMENT TRANSPORT; SEDIMENTATION; SIZE DISTRIBUTION; SUBMARINE CHANNEL;

AFRICA; ATLANTIC OCEAN; CAP TIMIRIS CANYON; MAURITANIA; NIGER RIVER; SENEGAL RIVER; SUB-SAHARAN AFRICA; WEST AFRICA;

EID: 34247610346     PISSN: 00253227     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.margeo.2007.02.005     Document Type: Article

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