ग्रेन्युलाइट इसके अंग्रेजी अर्थ का उदाहरण

The overall sequence is generally considered to be a granulite gneiss, which has undergone multiple deformations and multiple metamorphic episodes.

The Archaeans are mainly represented by the Charnockite group of rocks comprising garnetiferous granulite and the Khondalite group of rocks made up of quartzite and gneisses.

The rock is mainly gneisses, granulites, migmatites, amphibolites and banded iron formation, intruded by basis and ultra-basic bodies.

The metapelites are of granulite facies and the ultramafics are of greenschist facies and the enclosing gneisses represent amphibolites facies.

The rocks have experienced multiple metamorphic events at amphibolite or granulite conditions, resulting in often complete destruction of original igneous or sedimentary (protolith) textures.

Within the low-strain zones, the Dugel Gneiss exists as a medium-grained leucocratic metagranite with phenocrysts of K-feldspar which has recrystallized into granulite facies.

The rock is greasy-looking with annealed quartz and feldspar, and syn-granulite facies leucosomes cutting across metamorphic banding, and subsequently deformed by later metamorphism.

3350-3300 Ma; Amphibolite to granulite facies metamorphism.

The Western Gneiss Terrane is a series of polydeformed high-grade early Archaean metamorphic belts, composed predominantly of feldspathic leucocratic granulite gneisses, which represent some of the oldest crustal fragments on Earth.

The metamorphic grade is considered to be peak granulite facies, but the majority has preserved peak amphibolite facies assemblages.

Musgrave Block of granulite gneiss and igneous rocks.

The carbonate rocks are pure white, and coarsely crystalline and the deformed and banded marbles cover a triangular area of ; surrounded by diopside–scapolite–feldspar calc-granulites.