Abstract
Reports the occurrence of immature, mainly marine source, organic-carbon rich black shales of Albian to early Santonian and a major deep-sea fan sequence of Santonian to early Campanian age which was replaced by shallower facies. Paleogeographic, sediment source areas, sedimentation mechanism and rates, and biostratigraphic data are summarised.-after Authors
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APA
Hay, W. W., & Sibuet, J. C. (1984). Site 530: southeastern corner of the Angola Basin ( DSDP). Initial Reports DSDP, Leg 75, Walvis Bay to Recife. Part 1, 29–285. https://doi.org/10.2973/dsdp.proc.75.102.1984
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