Plume-driven recratonization of deep continental lithospheric mantle
Cratons are Earth’s ancient continental land masses that remain stable for billions of years. The mantle roots of cratons are renowned as being long-lived, stable features of Earth’s continents, but there is also evidence of their disruption in the recent 1 – 6 and more distant 7 – 9 past. Despite p...
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Veröffentlicht in: | Nature (London) 2021-04, Vol.592 (7856), p.732-736 |
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