It would remain metamorphic rock.
The metamorphic facies associated with the subduction of oceanic crust and sediments that forms under very high pressure and moderately low temperature is called the "blueschist facies." This facies typically develops at depths of around 15 to 30 kilometers, where the pressure is significantly high, but the temperatures remain relatively low compared to other metamorphic environments. The presence of minerals such as glaucophane and lawsonite characterizes this facies, indicating the unique conditions of subduction zones.
"Constant pressure" means the pressure must not change.
No. High pressure is pressure that is higher than an established normal pressure. The pressure may be rising, falling, or remain the same
In metamorphic rock, the texture and structure often remain consistent despite changes in mineral composition. This is due to the processes of heat and pressure that cause recrystallization, leading to the formation of new minerals while maintaining the original rock's overall fabric. Additionally, features like foliation or banding may persist, reflecting the original rock's characteristics.
pressure did not remain constant or if the amount of gas did not remain constant.
Intrusive igneous and metamorphic. Intrusive igneous rocks are those that solidify underground. Metamorphic rocks are those that are deep underground and subjected to intense heat and pressure, but remain a solid.
Do nothing. It is not necessary to do anything if you want a rock to remain the same.
Metamorphic rocks can turn into magma through a process called partial melting caused by high temperatures and pressure in the Earth's mantle. As the metamorphic rock is subjected to increased heat and pressure, some minerals within the rock may melt into magma while others remain solid. This process can lead to the formation of igneous rocks from the melted minerals.
During the formation of metamorphic rocks, high pressure and temperature can alter the minerals and textures of the rock, which can destroy any existing fossils. The recrystallization and deformation that occurs during metamorphism can erase or distort the original fossil structures. Additionally, the fluids involved in metamorphic processes can dissolve any organic material, further eliminating any fossil remnants.
The length of time is totally dependent to the conditions of heat and pressure under which the rock is exposed. Until certain conditions are met, the rock will remain a solid.
No. Bottlenose dolphins remain in the same form their whole life but grow in size.
Of course they can. The overall compositions of the rocks will remain the same (assuming a closed system, which isn't always the case), but mineralogically there will be changes due to metamorphic pressures and temperatures. There are a whole list of minerals which only formed from metamorphic processes.
"Constant pressure" means the pressure must not change.
No. High pressure is pressure that is higher than an established normal pressure. The pressure may be rising, falling, or remain the same
In metamorphic rock, the texture and structure often remain consistent despite changes in mineral composition. This is due to the processes of heat and pressure that cause recrystallization, leading to the formation of new minerals while maintaining the original rock's overall fabric. Additionally, features like foliation or banding may persist, reflecting the original rock's characteristics.
pressure did not remain constant or if the amount of gas did not remain constant.
Applying a pressure on sodium chloride this remain solid; but the allotropic forms are changed.