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.
A foiliated metamorphic rock is a metamorphic rock that has a texture of parallel alignment of mineral grains. Your Welcome...
no texture
Metamorphic rocks that consist of only one mineral that forms large interlocking crystals often have a _____ texture.
A porphyritic texture is displayed in an igneous rock containing large isolated crystals (phenocrysts) in a mass of fine textured crystals . Porphyritic texture indicates that a magma has gone through a two stage cooling process. The magma has cooled sufficiently underground to allow some minerals to crystallize and grow in size; the magma is then expelled above ground where the remaining liquid magma solidifies quickly, allowing only small crystals to develop.See link below for a picture of a porphyritic texture in a rock.
A schistose texture.
A foiliated metamorphic rock is a metamorphic rock that has a texture of parallel alignment of mineral grains. Your Welcome...
A folliated texture metamorphic rock, like shist.
Yes
And their texture, which can be aphanitic, phaneritic, glassy, or porphyritic. mineral composition and crystal texture
no texture
No banding or alignment of a metamorphic rock's minerals would be consider non-foliated.
no texture
Porphyritic texture is a feature of some igneous rocks, not sedimentary rocks.
Metamorphic rocks that consist of only one mineral that forms large interlocking crystals often have a _____ texture.
Metamorphic rocks that consist of only one mineral that forms large interlocking crystals often have a _____ texture.
mineral grains arranging into layers.
A porphyritic texture is displayed in an igneous rock containing large isolated crystals (phenocrysts) in a mass of fine textured crystals . Porphyritic texture indicates that a magma has gone through a two stage cooling process. The magma has cooled sufficiently underground to allow some minerals to crystallize and grow in size; the magma is then expelled above ground where the remaining liquid magma solidifies quickly, allowing only small crystals to develop.See link below for a picture of a porphyritic texture in a rock.