About: Plating (geology)

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In geology, plating is a hypothesized process whereby asthenospheric mantle hardens beneath crustal material, thereby becoming attached to it and thereafter moving together with the crustal material as part of the lithosphere. A complementary process, although it does not necessarily always involve the upper mantle, is called delamination.

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  • In geology, plating is a hypothesized process whereby asthenospheric mantle hardens beneath crustal material, thereby becoming attached to it and thereafter moving together with the crustal material as part of the lithosphere. A complementary process, although it does not necessarily always involve the upper mantle, is called delamination. (en)
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  • In geology, plating is a hypothesized process whereby asthenospheric mantle hardens beneath crustal material, thereby becoming attached to it and thereafter moving together with the crustal material as part of the lithosphere. A complementary process, although it does not necessarily always involve the upper mantle, is called delamination. (en)
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  • Plating (geology) (en)
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