Sillimanite is an index mineral for high temperature and variable pressure metamorphism.
It is a medium-grade metamorphic rock with a preponderance of the platy mineral graphite.
Gneiss is usually considered a high grade metamorphic rock (although there are some weird exceptions).
Both gneiss and migmatite are late-stage, high grade metamorphic rocks.
A high metamorphic grade
Sillimanite is an index mineral for high temperature and variable pressure metamorphism.
Garnet is a mineral most often found in high grade metamorphic rock.
high grade metamorphism can progress to pressure and weather.
It is a medium-grade metamorphic rock with a preponderance of the platy mineral graphite.
Gneiss is usually considered a high grade metamorphic rock (although there are some weird exceptions).
Metamorphic rock can undergo a series of changes called degrees of metamorphism, from low-grade to high-grade.
Yes! since index minerals form at specific pressure and temperature conditions hence when they are encountered or observed in a certain metamorphic rock they serve to indicate the condition by which the rock formed.They can tell whether it is a high grade or low grade metamorphism.e.g Andalusite mineral indicate high grade metamorphism associated with high temperature.
Greenschist, blueschist, zeolite, granulite and eclogite high grade metamorphic rocks.
It's eclogite facies.
Both gneiss and migmatite are late-stage, high grade metamorphic rocks.
Schist is a high-grade metamorphic rock.
it is formed by high-grade regional metamorphic processes