Heat And Pressure
The two main groups of metamorphic rocks are foliated and non-foliated. Foliated metamorphic rocks show layering and parallel alignment of flat mineral crystals (ex. micas). The "banded texture in metamorphic rocks" is one of the specific kinds of foliated textures. It is referred to as gneissic banding. Essentially, this texture displays alternating layers of light and dark minerals. These rocks are called gneiss- the light bands form from quartz and feldspars, while the dark ones form from ferromagnesian minerals.
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Granite is an igneous rock and gneiss is a metamorphic rock.
Heat And Pressure
Heat and pressure cause granite to change to gneiss.
Granite gneiss is a metamorphic rock and would not be considered extrusive (rock formed from molten material at or near the surface).
A gneiss is a metamorphic rock. Metamorphic rocks are created by the alteration of rocks by heat and pressure. Therefore, a gneiss may be created from an igneous rock in which case it would be called an orthogneiss.
A banded metamorphic rock formed from the re-heating and re-pressuring of granite and similar igneous rocks.
Gneiss
Slate and gneiss are examples of metamorphic rock.
Granite is Igneous rock. It crystallizes from hot melt (magma). Metamorphic rocks can be found associated with granite as result of their contact with country (surrounding) rocks. This will be a contact metamorphism. Metamorphism of granite it self results into granitic gneisses which are coarse foliated rocks.
Igneous:GraniteBasaltDioriteObsidianRhyolitePumiceMetamorphic: SlateMica SchistQuartziteGabbroMarblePhylliteMetaconglomerateSkarnSedimentary:LimestoneChalkCoquinaShaleSandstoneMudstoneConglomerateBreccia
Granite is an intrusive igneous rock, meaning it has solidified underground as opposed to solidification on the surface.
Both igneous and metamorphic rocks are formed by pressure and some kind of heat