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International symposium on deep internal processes and continental rifting(dipcr)1985, china: abstracts, Sept. 9-13, 1985, Chengdu, China
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摘要
Rift valleys commonly form on high plateaus underlain by the low-velocity and low-density anomalous mantle. The buoyancy force from the anomalous mantle keeps the crust in a highly elevated position whichsproduces high additional stresses in the lithosphere.

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