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The thickness of continental crust is not only thicker but also less dense than that of oceanic crust. The average thickness of the continental crust is thirty-five kilometers, though it may be considerably thicker or thinner in particular regions.
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大陆壳的厚度比洋壳大,但密度小于洋壳。陆壳的平均厚度为35公里左右,局部地区有增厚和减薄现象。
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