Phyllite is metamorphosed slate, which is also a metamorphic rock. Shale or mudstone is the protolith (parent rock) of slate.
phyllite
Phyllite is a type of metamorphic rock that forms from the metamorphism of slate. It is characterized by its sheen, fine-grained texture, and foliated structure.
If slate is sufficiently heated and compressed it becomes phyllite.
Shale undergoes metamorphism and transforms into slate, then phyllite, followed by schist, and eventually gneiss as heat and pressure increase. This progression represents a sequence of increasing metamorphic grade from low (slate) to high (gneiss) with changes in mineral composition and texture.
Phyllite is formed from the metamorphism of shale or mudstone. During this process, the minerals in the original rock recrystallize and align in a parallel structure, giving phyllite its characteristic foliated texture. The increased heat and pressure cause the minerals to reorganize, forming a fine-grained texture with a silky sheen.
Phyllite is metamorphosed slate, which is also a metamorphic rock. Shale or mudstone is the protolith (parent rock) of slate.
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.
Slate is a fine-grained metamorphic rock formed from the low-grade metamorphism of shale or mudstone, while phyllite is a more intermediate-grade metamorphic rock formed from the metamorphism of slate. Phyllite has a more pronounced foliation and sheen due to increased metamorphic pressure and temperature compared to slate.
phyllite
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.
Phyllite is a type of metamorphic rock that forms from the metamorphism of slate. It is characterized by its sheen, fine-grained texture, and foliated structure.
If slate is sufficiently heated and compressed it becomes phyllite.
slate
Shale undergoes metamorphism and transforms into slate, then phyllite, followed by schist, and eventually gneiss as heat and pressure increase. This progression represents a sequence of increasing metamorphic grade from low (slate) to high (gneiss) with changes in mineral composition and texture.
Phyllite is a foliated metamorphic rock that is texturally intermediate between slate and schist. It exhibits a greater degree of metamorphism than slate but not as much as schist, resulting in a medium-grain texture with a glossy sheen.
yes, it's slate. it goes from shale to slate to phyllite to mica schist.