high grade metamorphism can progress to pressure and weather.
Metamorphic rock can undergo a series of changes called degrees of metamorphism, from low-grade to high-grade.
Gneiss is typically associated with high-grade metamorphism, which means that it has undergone intense heat and pressure to form distinct banding of minerals. This places gneiss in the high-pressure and high-temperature conditions of the regional metamorphic grade.
Slate is a low-grade metamorphic rock characterized by fine-grained foliated structure. Phyllite is intermediate-grade metamorphic rock with a greater degree of crystallization and foliation than slate. Schist is a medium-grade metamorphic rock with visible mineral grains and strong foliation. Gneiss is a high-grade metamorphic rock with distinct banding of light and dark minerals and high crystallization.
Greenschist, blueschist, zeolite, granulite and eclogite high grade metamorphic rocks.
It's eclogite facies.
it is formed by high-grade regional metamorphic processes
Schist is a high-grade metamorphic rock.
Both gneiss and migmatite are late-stage, high grade metamorphic rocks.
Yes. Most likely it would become a metamorphic rock of higher grade. Slate is a low grade metamorphic rock. With increased heat and pressure it will become schist, a high grade metamorphic rock.
Garnet is a mineral most often found in high grade metamorphic rock.
Granulite forms at the highest grade of regional metamorphism. It is a high-grade metamorphic rock primarily composed of minerals such as pyroxene and plagioclase feldspar. Granulite typically forms under high temperatures and pressures deep within the Earth's crust.
Sillimanite is an index mineral for high temperature and variable pressure metamorphism.