 | This article needs additional citations for
verification. (April 2010) |
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. [1]
A complementary process, although it does not necessarily always involve the upper mantle, is called delamination.
See also
References
- ^ Frank Press; Raymond Siever; John Grotzinger; Thomas Jordan; Volker Schweizer (2017). Allgemeine Geologie (in German). Berlin, Heidelberg: Springer Spektrum. p. 23 f. ISBN 978 3 662 48341 1.
 | This tectonics article is a stub. You can help Wikipedia by expanding it. |
| This article needs additional citations for
verification. (April 2010) |
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. [1]
A complementary process, although it does not necessarily always involve the upper mantle, is called delamination.
See also
References
- ^ Frank Press; Raymond Siever; John Grotzinger; Thomas Jordan; Volker Schweizer (2017). Allgemeine Geologie (in German). Berlin, Heidelberg: Springer Spektrum. p. 23 f. ISBN 978 3 662 48341 1.
|
| This tectonics article is a stub. You can help Wikipedia by expanding it. |