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• W2058439972 abstract "The Atlantic Mesozoic rift system consists of four branches separated from one another by fracture zones. Morphologically it resembles the ridge transform-ridge topography of mid-ocean ridges. The branches include the northern North Atlantic between the New foundland/Gibraltar and Bahamas/Guinea fracture zones, the Southern North Atlantic between the Bahama/Guinea and Equatorial fracture zones, the Equatorial Atlantic between the Equatorial Fracture zone and the Torres/Walvis Ridge, and the South Atlantic between the Torres/Walvis Ridge, and the Falkland/Agulhas Fracture Zone. The fundamental structure along the shear zones is the graben, and within the rift branches the half graben. Rifting began in Late Triassic at the northern end of the Northern North Atlantic Branch in the Early Jurassic at the South Atlantic Branch. The rifts propagated toward one another cutting through the equatorial region sometime in latest Middle Jurassic. Seafloor spreading at the northern end of the Northern North Atlantic Branch began in Middle Jurassic reaching the Bahama/Guinea Fracture Zone toward the end of Middle Jurassic. Seafloor spreading in the South Atlantic Branch in the early Aptian and in the Equatorial Atlantic Branch in the Albian. A continuous North/South Atlantic oceanic basin was formed with the separation of the African and South American continents in the Turonian." @default.
• W2058439972 created "2016-06-24" @default.
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• W2058439972 date "1989-01-01" @default.
• W2058439972 modified "2023-10-14" @default.
• W2058439972 title "The tectonic style of the atlantic mesozoic rift system" @default.
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• W2058439972 doi "https://doi.org/10.1016/s0899-5362(89)80021-1" @default.
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