Deep, ultra-hot-melting residues as cradles of mantle diamond
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Modelled compositions residues after melting of basalt-peridotite
Deep ultra-hot Archaean mantle dynamics; highly depleted residues as cradles for mantle diamond
컨텐츠 Nature Portfolio
Trace-element compositions (in ppm) of the source used in our model
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Lithosphere thickness controls the extent of mantle melting, depth of melt extraction and basalt compositions in all tectonic settings on Earth – A review and new perspectives - ScienceDirect
Depth-dependent peridotite-melt interaction and the origin of variable silica in the cratonic mantle
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The geothermal gradient of the Kaapvaal craton at the time of
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Formation of Archaean continental lithosphere and its diamonds: the root of the problem
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Formation of Archaean continental lithosphere and its diamonds: the root of the problem
