Anatexis

Anatexis (via Latin from Greek roots meaning "to melt down") is the partial melting of rocks.^[1] Traditionally, anatexis is used specifically to discuss the partial melting of crustal rocks, while the generic term "partial melting" refers to the partial melting of all rocks, in both the crust and mantle.^{[citation needed]}

Anatexis can occur in a variety of different settings, from zones of continental collision to mid-ocean ridges.^[2] It is believed that anatexis is the process largely responsible for the formation of migmatites.^[1] Furthermore, scientists have recently discovered that partial melting plays an increasingly important role in active crustal processes, including the advancement of active deformation and the emplacement of crustal granites.^[3] As a result, active feedback between crustal shearing, melting, and granite emplacement^[3] has become largely accepted in the place of large scale, unreasonable models involving fractional melting of the mantle into granitic batholiths and plutons.^[4] Evidence for this can be seen in the physical, mineralogical, and isotopic signatures of countless granites.^[5]