Distinguishing between fine‐grained turbidites and contourites on the Nova Scotian deep water margin

Sedimentology

Volumn 26, Issue 3, 1979, Pages 371-387

  STOW, DORRIK A V ^a  

^a DALHOUSIE UNIVERSITY   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 84984038201     PISSN: 00370746     EISSN: 13653091     Source Type: Journal    
DOI: 10.1111/j.1365-3091.1979.tb00915.x     Document Type: Article

References (79)

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4. Distribution, composition and transport of suspended sediment in Redondo submarine canyon and vicinity (California)
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16. The Western North Atlantic
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21. Sedimentation in Cascadia deep sea channel
22. Shaping of the continental rise by deep geostrophic contour currents
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24. Contour currents in the Weddell Sea
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27. Textural evidence for the deposition of many western north Atlantic deep sea sands by ocean‐bottom currents rather than turbidity currents
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54. Deep bottom currents off the coast of North Carolina
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56. Further evidence of contour currents in the western north Atlantic
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60. Pulsating turbidity currents with relationship to high swell and high tides
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67. Sediments of the New England continental rise