No. Contact metamorphism will most likely alter shale into hornfels. Phyllite is regionally metamorphosed slate, and slate is metamorphosed shale.
Contact Metamorphism
contact metamorphism, regional metamorphism, dynamic metamorphism
contact and regional metamorphic are similar because both of them happen cause of hot heat and pressure which make the rock metamorphic
Burial metamorphism differs from regional and contact metamorphism in that it is the result of rocks being buried deeper into the earth's crust through tectonic movements.
No. Contact metamorphism will most likely alter shale into hornfels. Phyllite is regionally metamorphosed slate, and slate is metamorphosed shale.
Slate is the metamorphic rock, formed from regional (heat and pressure applied) metamorphism on shale.
Shale.
Shale (a sedimentary rock) transforms naturally into slate (a metamorphic rock) after millions of years of burial deep in the crust under high temperature and pressure. It it not possible to artificially transform shale into slate.
contact :)
shale and sandstone
Contact Metamorphism
Very low grade regional metamorphism.
Hornfels
contact metamorphism, regional metamorphism, dynamic metamorphism
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.
Timothy C. Hester has written: 'Log-derived regional source-rock characteristics of the Woodford Shale, Anadarko Basin, Oklahoma' -- subject(s): Anadarko Basin, Geology, Oklahoma, Shale, Stratigraphic Geology