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Rapid transition from primary to secondary crust building on the Moon explained by mantle overturn - Nature Communications

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Rapid transition from primary to secondary crust building on the Moon explained by mantle overturn - Nature Communications

Geochronology indicates a rapid transition (tens of Myrs) from primary to secondary crust building on the Moon. The processes responsible for initiating secondary magmatism, however, remain in debate. Here we test the hypothesis that the earliest secondary crust (Mg-suite) formed as a direct consequence of density-driven mantle overturn, and advance 3D mantle convection models to quantify the resulting extent of lower mantle melting.

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Rapid transition from primary to secondary crust building on the Moon explained by mantle overturn - Nature Communications

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Rapid transition from primary to secondary crust building on the Moon explained by mantle overturn - Nature Communications

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