Abstract
The first marine incursion of the incipient North Atlantic Ocean is recorded in the uppermost Triassic to Lower Jurassic sequence. A lithologic change from continental red beds below to slope breccias and hemipelagic carbonates above indicates that a carbonate ramp was probably established by Sinemurian time along the Moroccan continental margin and that subsidence in the adjacent basin was rapid in the early phases of continental rift.-from Author
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CITATION STYLE
Reigraf, W., Luterbacher, H., & Leckie, R. M. (1984). Jurassic foraminifers from the Mazagan Plateau, Deep Sea Drilling Project Site 547, Leg 79, off Morocco. Initial Reports DSDP, Leg 79, Las Palmas to Brest, 671–702. https://doi.org/10.2973/dsdp.proc.79.126.1984
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