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Trondhjemite

Trondhjemites are leucotonalites, a variety of leucocratic tonalite in which the modal mineralogy mostly consists of plagioclase in the form of albite to andesine, >20% quartz, and <10% alkali feldspar. Trondhjemites that occur in the oceanic crust or in ophiolites are usually called plagiogranites.

Formation
Generation of trondhjemite-tonalitic magmas are understood be caused by fractionation of wet basaltic and/or dry low-K tholeiitic-andesitic magmas caused by partial melting of quartz eclogites, amphibolites or gabbros. ==Notes==
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