No. The metamorphism of shale forms slate. Granite is formed when high-silica magma cools underground.
No . Shale is formed my the metamorphism of the rock - Slate
Hydrothermal metamorphism of a granite prototype.
No. Contact metamorphism will most likely alter shale into hornfels. Phyllite is regionally metamorphosed slate, and slate is metamorphosed shale.
Contact Metamorphism
Shale is a sedimentary rock that can transform into other types of rock through the process of metamorphism. Under heat and pressure, shale can turn into slate, while further metamorphism can result in the formation of phyllite, schist, and gneiss.
No . Shale is formed my the metamorphism of the rock - Slate
Slate is the metamorphic rock, formed from regional (heat and pressure applied) metamorphism on shale.
Hydrothermal metamorphism of a granite prototype.
shale and sandstone
Contact metamorphism takes place locally near igneous intrusions. It is caused by low to moderate pressure, intense heat, and reactions to magma that is being metamorphosed. When contact metamorphism takes place with mudstone or shale (sedimentary rocks) slate is formed. The mudstone or shale is the parent rock or protolith.
The parent rock for slate is shale.
Shale is a sedimentary rock. In increasing metamorphism, the sequence begins with shale and leads to phyllite, schist, then gneiss.
No. Contact metamorphism will most likely alter shale into hornfels. Phyllite is regionally metamorphosed slate, and slate is metamorphosed shale.
Granite is Igneous rock. It crystallizes from hot melt (magma). Metamorphic rocks can be found associated with granite as result of their contact with country (surrounding) rocks. This will be a contact metamorphism. Metamorphism of granite it self results into granitic gneisses which are coarse foliated rocks.
Contact Metamorphism
No. its the opposite. gneiss forms after shale goes through metamorphism
No. Granite is an intrusive igneous rock, formed from the solidification of magma underground. Slate is a low grade metamorphic rock formed from heat and pressure applied to deposits of shale, a sedimentary rock.