Decompression Melting is a geological process in the context of magma genesis whereby mantle material undergoes partial melting due to a decrease in pressure accompanying uplift in the absence of significant heat or volatile addition, distinguishing it from flux and heat-induced melting mechanisms.
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Experimental Constraints on Himalayan Anatexis
Alberto E. Patiño Douce, Nigel Harris · Journal of Petrology · 1998 · 1K citations
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The University of Tokyo
Tokyo, Japan
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Chinese Academy of Sciences
Beijing, China
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Canberra, Australia
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California Institute of Technology
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