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Models for Quantifying Mantle Melting Processes

2014
Partial 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
openaire   +1 more source

Partial Melting and Melt Segregation in a Convecting Mantle

2000
Various 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.
openaire   +1 more source

Deep Eutectic Solvents: A Review of Fundamentals and Applications

Chemical Reviews, 2021
Brian Chen, Yong Zhang, Jeffrey M Klein
exaly  

Kimberlites: complex mantle melts

Deep Sea Research Part B. Oceanographic Literature Review, 1984
openaire   +2 more sources

Melt in Mantle

Science, 2008
openaire   +1 more source

Mantle plumes and their role in Earth processes

Nature Reviews Earth & Environment, 2021
Anthony A P Koppers   +2 more
exaly  

Mantle Melt Mixing

Science, 2007
openaire   +1 more source

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