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Seafloor spreading - Wikipedia, the free encyclopedia
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Sea floor spreading is one component of the theory of plate tectonics. According to this concept, at ridges in many of the world's oceans (mid-ocean ridges), new crustal rock is added to the edges ... Using the age of the rock you have chosen and its distance from the MAR, calculate the half-rate of sea floor spreading,
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See J. Coulomb, Sea Floor Spreading and Continental Drift (1972) ... Age of oceanic crust; youngest (red) is along spreading centres. ... Plates in the crust of the earth, according to the plate tectonics theory...
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DESCRIPTION: "Ring of Fire", Plate Tectonics, Sea-Floor Spreading, Subduction Zones, "Hot Spots" ... According to the new, generally accepted "plate-tectonics" theory, scientists believe that the Earth's surface is broken into a number of shifting slabs or plates, which average about 50 miles in thickness.
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According to Wegner, about 200 million years ago, all the continents had been joined in a single ... Stripes of approximately the same size should be carried away from either side of the ridge as spreading pulls the new oceanic crust apart. Sea-floor spreading is also supported by the age of the seafloor.
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Brightness contrasts mark a discontinuity in plate age and thus in plate thickness. The brightness contrast on one side of ... We have shown that a wax model of sea-floor spreading, under the right conditions, produces tectonic microplates that evolve in time according to a kinematic model designed for oceanic microplates.
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Thus, serpentinization and unroofing were time-transgressive and the age of the non-volcanic sea floor formed by the unroofed mantle grows younger outboard, just as is the case for normal, volcanic sea floor.
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