A porphyritic texture can be a feature of igneous rocks, but 'porphyritic' is not used to describe metamorphic rock texture. Metamorphic rocks can be foliated or non-foliated, terms used to describe mineral alignment or banding, or the lack thereof.
Phyllite is a type of metamorphic rock, not a mineral. It is formed from the metamorphism of shale or mudstone and has a fine-grained texture with a silky sheen due to the alignment of its minerals.
A foliated metamorphic rock is a rock that has a layered or banded appearance due to the alignment of minerals in parallel planes. This alignment is typically a result of the rock being subjected to high pressure and temperature conditions during its formation. Examples include gneiss and schist.
The temperature and pressure conditions during metamorphism can affect the texture of metamorphic rock. Higher temperatures and pressures typically lead to a more pronounced foliation and mineral alignment, resulting in a finer texture. Additionally, the presence of fluids during metamorphism can also influence the development of specific textures in metamorphic rocks.
A type of metamorphic rock similar to granite is gneiss. Gneiss is a foliated metamorphic rock that has a similar composition to granite but displays a banded texture due to the alignment of mineral grains during metamorphism.
no texture
Schist is a metamorphic rock that exhibits parallel alignment of mineral grains, giving it a foliated appearance. This alignment is typically a result of regional metamorphism where intense pressure and temperature conditions cause the minerals to recrystallize in a preferred orientation.
Phyllite is a type of metamorphic rock, not a mineral. It is formed from the metamorphism of shale or mudstone and has a fine-grained texture with a silky sheen due to the alignment of its minerals.
When a metamorphic rock exhibits a layered or banded appearance, it is said to exhibit foliated texture. This texture is a result of the alignment of mineral grains or the presence of alternating light and dark layers. Examples of foliated metamorphic rocks include gneiss and schist.
A foliated metamorphic rock is a rock that has a layered or banded appearance due to the alignment of minerals in parallel planes. This alignment is typically a result of the rock being subjected to high pressure and temperature conditions during its formation. Examples include gneiss and schist.
no texture
Metamorphic rocks with a non-foliated texture show that the metamorphic changes involved did not result in the development of a preferred alignment of mineral grains. This indicates that the rocks were subjected to directed pressure or high temperatures without causing the minerals to align into layers. Examples of non-foliated rocks include marble and quartzite.
No banding or alignment of a metamorphic rock's minerals would be consider non-foliated.
The temperature and pressure conditions during metamorphism can affect the texture of metamorphic rock. Higher temperatures and pressures typically lead to a more pronounced foliation and mineral alignment, resulting in a finer texture. Additionally, the presence of fluids during metamorphism can also influence the development of specific textures in metamorphic rocks.
Yes, a porphyritic texture consists of two distinct sizes of mineral grains - larger crystals called phenocrysts surrounded by a finer-grained matrix called groundmass. This texture typically forms in magmas that experience two stages of cooling, resulting in the different sizes of crystals.
A metamorphic rock can be classified according to its texture, mineral composition, and metamorphic grade. Texture refers to the size and arrangement of mineral grains, while mineral composition indicates the minerals present. Metamorphic grade refers to the temperature and pressure conditions under which the rock formed.
A type of metamorphic rock similar to granite is gneiss. Gneiss is a foliated metamorphic rock that has a similar composition to granite but displays a banded texture due to the alignment of mineral grains during metamorphism.
no texture