theory of plate tectonics oor Spaans
theory of plate tectonics
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tectónica de placas
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This was, or course, long before the theory of plate tectonics.
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Would this support or refute the theory of plate tectonics?
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Under this theory of plate tectonics, continental drift is an inescapable consequence.
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The theory of plate tectonics provided a unifying idea for many different aspects of geology.
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The theory of plate tectonics in geology explains the phenomenon of continental drift.
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The theory of plate tectonics has led us to reconstruct the history of our planet’s surface.
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How does the theory of plate tectonics help us understand the causes of ice ages?
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It was resurrected in the 1960s as part of the theory of PLATE TECTONICS.
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With the development of the theory of plate tectonics, the picture was greatly clarified.
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The theory of plate tectonics is still only a theory.”
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Scientists try to explain by using the theory of plate tectonics.
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� Does the theory of plate tectonics explain alternating glacial–interglacial climates during the Pleistocene?
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This book covers the unified by the theory of plate tectonics, which has revolutionized our studies in geology.
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That is, in summary, the modern theory of plate tectonics.
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The second was the theory of plate tectonics, which helped make sense of the geographical distribution of ancient life.
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According to the theory of plate tectonics, however, the entire surface of the earth is divided into several large plates.
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The crater was named after the German geophysicist, polar researcher and meteorologist Alfred Wegener, originator of the theory of Plate tectonics.
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But the way it happened, according to the theory of plate tectonics, is a bit different from the way Wegener saw it.
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In older geological works predating theories of plate tectonics, the United States' Catskill Delta formation is sometimes referred to as part of the Old Red Sandstone.
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The theory of plate tectonics demonstrates that the continents of the Earth are moving across the surface at the rate of a few centimeters per year.
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Some of the most significant advances in 20th-century geology have been the development of the theory of plate tectonics in the 1960s and the refinement of estimates of the planet's age.
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The creation of polymetallic sulphide deposits starts at active vent sites, and over time the deposits grow in size and shift away from the active venting in accordance with the theory of plate tectonics.
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Broadly speaking, the theory of plate tectonics says that earthquakes and volcanoes will occur in similar regions —in rifts, especially oceanic rifts; in earth’s crust, where magma rises from the mantle through fissures; and at subduction zones, where one plate plunges under another.
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The growth of other disciplines, such as geophysics, in the 20th century, led to the development of the theory of plate tectonics in the 1960s, which has had a similar effect on the Earth sciences as the theory of evolution had on biology.
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“The theory of plate tectonics seems to provide answers for so many questions that we are tempted to believe it is the long-sought unifying theory that explains the lithosphere [the land areas of the earth, from its surface to the center of the earth].
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