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Both gneiss and migmatite are late-stage, high grade metamorphic rocks.
The parent rock of migmatite is typically a metamorphic rock like gneiss or schist that has undergone partial melting due to high temperatures and pressures. This partial melting results in the formation of a mixed rock composed of both igneous and metamorphic features.
Gneiss is a Plutonic metamorphic rock which is formed under high pressure and temperature condition at Katazone or Lower Zone.
Altered varieties of granite formed during the cooling period include gneiss, schist, and migmatite. These rocks are created when the original granite undergoes intense heat and pressure, causing recrystallization and alteration of the minerals in the rock.
If slate is subjected to even more pressure, it can undergo metamorphism, transforming into schist or gneiss, depending on the conditions of temperature and pressure. This process alters its mineral composition and texture, resulting in a more foliated or banded appearance. Ultimately, with sufficient heat and pressure, it may further evolve into granite or even migmatite if melting occurs.
thee color of migmatite is green and white
Migmatite.
Normally you don't use it by it's self. it is combined with other things. It is found in fish and birds and even brains sometimes. look on wikipedia. that is where I'm giving you this information from.
migmatite
Difficult to give you a precise answer, migmatites are composed of a leucosome which is new material crystallized from incipient melting and a mesosome which is old material that resisted melting. These two materials may form a fine fabric which imparts a foliation to the rock. The leucosome may also be incoherently folded. Also if the migmatite is forming from a foliated source, the foliation may persist. Thus migmatites are metamorphic rocks that show characteristics of incipient melting and they may or may not show a foliation too, the foliation is not a critical characteristic of a rock being a migmatite.
Both gneiss and migmatite are late-stage, high grade metamorphic rocks.
The parent rock of migmatite is typically a metamorphic rock like gneiss or schist that has undergone partial melting due to high temperatures and pressures. This partial melting results in the formation of a mixed rock composed of both igneous and metamorphic features.
Karl Richard Mehnert has written: 'Migmatites and the origin of granitic rocks' -- subject(s): Migmatite
Possibly shale, as it goes through a series of metamorphic transitions from slate to migmatite.
igneous
Yes, granite can be banded in appearance due to the presence of different minerals and variations in the cooling process during its formation. These bands are typically called gneiss or migmatite.
At the point of total melt, it would be called magma. Metamorphic rock that exhibits partial melting is called migmatite.