| Igneous rock | |
| Tonalite–trondhjemite–granodiorite migmatite (left) and trondhjemitic gneiss (right) from northern China | |
| Composition | |
|---|---|
| oligoclase, other plagioclase |
Trondhjemite is a leucocratic (light-colored) intrusive igneous rock. It is a variety of tonalite in which the plagioclase is mostly in the form of oligoclase. [1] Trondhjemites that occur in the oceanic crust or in ophiolites are usually called plagiogranites. [2] [3]
Trondhjemite is common in Archean terranes occurring in conjunction with tonalite and granodiorite as the TTG (tonalite–trondhjemite–granodiorite) orthogneiss suite. [4] Trondhjemite dikes also commonly form part of the sheeted dike complex of an ophiolite. [3]
The rock type was first described by Victor Goldschmidt in 1916. The name of the rock type is derived from the city of Trondheim, Norway. [1]