Examination of downhole variation in % organic C %, thickness of black sediment, radiolarian sand (radiolarite layers) frequency, % thickness of calcareous mudstone, and graded unit frequency, suggests 1) major organic productivity control of blackness and C content, 2) local variation in CCD level, and 3) some turbidite deposition for Sites 386 and 387. -Author
CITATION STYLE
McCave, I. N. (1979). Depositional features of organic- carbon-rich black and green mudstones at DSDP Sites 386 and 387, western North Atlantic. Initial Reports of the Deep Sea Drilling Project, Leg 43, Istanbul, Turkey to Norfolk, Virginia, 1975, (Scripps Institution of Ocenaography; UK Distributors IPOD Commitee, NERC, Swindon), 411–416. https://doi.org/10.2973/dsdp.proc.43.110.1979
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