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Rift - Wikipedia, the free encyclopedia
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Rift valley - Wikipedia, the free encyclopedia
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In the long geological time period up to the end of the Carboniferous, almost all of Nova Scotia's geological units -- the old crystalline rocks of the Avalon Zone and the folded slates and greywackes of the Meguma Zone, along with younger Devonian ... Morphology of the Triassic-Jurassic Area; Continental Separation...
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It explains the Site 900 MORB gabbro as material underplated beneath thinned continental crust or as an aborted point-of-initiation of seafloor spreading, and the alkaline to transitional characters of igneous clasts in Site 897 and 899 deposits as evidence of continental rifting.
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Looking for something in particular? the entire directory only this category ... More search options ... Home : Earth Science : Geology : Plate Tectonics : Continental Rifting...
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Nonetheless, differences in the magnitude of seafloor spreading are systematically compensated by differences in the magnitude of continental extension, which was calculated by reconstructing thinned continental crust to its pre-rifting thickness.
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Cretaceous continental rifting that led to separation of Africa and South America was associated with mantle plume activity (Tristian plume) and bimodal volcanic-plutonic magmatism in southwestern Africa and Atlantic margin in South America.
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