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Models for Quantifying Mantle Melting Processes
2014Partial melting of mantle and crustal rocks is an important process for the genesis of a suite of igneous rocks seen at the surface of the earth. These rocks preserve the imprints of the complex physico-chemical processes in the earth’s interior in the form of their distinct end-member geochemical and isotopic compositions.
R. N. Singh, A. Manglik
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Partial Melting and Melt Segregation in a Convecting Mantle
2000Various causes for mantle melting (decompression, heating or release of water) combined with current estimates of upper mantle temperatures and the state of stress in the lithosphere suggest that in many regions the asthenosphere might be partially molten, but melts may not always be able to rise to the surface.
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Deep, ultra-hot-melting residues as cradles of mantle diamond
Nature, 2023Carl Walsh, Balz Kamber
exaly
Kimberlites: complex mantle melts
Deep Sea Research Part B. Oceanographic Literature Review, 1984openaire +2 more sources

