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.
Phyllite is metamorphosed slate, which is also a metamorphic rock. Shale or mudstone is the protolith (parent rock) of slate.
The luster of rock salt is Vitreous (glassy)
It depends on the rock.
You would need to look at the individual minerals. A rock does not have a luster.
Phyllite is a metamorphic rock.
Phyllite is a fine-grained metamorphic rock characterized by its silky sheen and flat, sheet-like structure due to the alignment of its mineral grains. It typically has a glossy to dull luster and often displays a pronounced foliation resulting from the parallel alignment of minerals like mica and chlorite. Phyllite can range in color from gray to green or black, depending on the presence of specific minerals.
Texture and metamorphic grade. Schist has visible crystals, while phyllite has crystals too small to be seen with the eye or barely seen. This is a result of schist having higher grade metamorphism.
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.
Phyllite is metamorphosed slate, which is also a metamorphic rock. Shale or mudstone is the protolith (parent rock) of slate.
Phyllite.
Phyllite is a metamorphic rock that forms from the parent rock shale or mudstone through low-grade metamorphism. During this process, the minerals in the original rock recrystallize and align, giving phyllite its characteristic silky sheen and foliated texture. The high pressure and moderate heat conditions required for the formation of phyllite result in the development of fine-grained mica minerals such as muscovite or biotite within the rock.
Phyllite is a type of metamorphic rock that comes from adding heat, pressure, and/or chemically active fluids to slate. Slate is the parent, or originial, type of rock from which the phyllite forms. It could also be said that slate recrystallizes into phyllite. Slate is also a metamorphic rock that starts out as the sedimentary rock called shale. Therefore, phyllite comes from slate, which comes from shale. Phyllite is different from slate because it has been metamorphosed more. As a result, the straight lines/planes (called foliation) that slate breaks along, are absent in phyllite, which is distinctly wavy in appearance. If more metamorphism is applied to phyllite, it recrystallizes into schist.
Not a mineral but a rock. Schist comes asfter phyllite ut before gneiss.
Probably the metamorphic rock phyllite.
Phyllite is foliated.
The protolith of phyllite is shale or mudstone that has been subjected to low-grade metamorphism. This metamorphic process causes the rock to recrystallize, resulting in a foliated texture with fine-grained mica minerals like muscovite and chlorite.