Describe the change in grain size from slate to Phyllite to schist.

Applications and Investigations in Earth Science (9th Edition)
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ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
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Describe the change in grain size from slate to Phyllite to schist. 

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Introduction:

Metamorphism can be understood as a process in which preexisting rock alters due to temperature pressure and chemically active fluid and the product is known as a metamorphic rock. The metamorphic processes begin after diagenesis (temperature range 100-150oC) and zeolite is considered as a transition between the sedimentary and metamorphic rock. The metamorphism retains up to 800-1000oC and above this temperature igneous processes begin, Migmatites considered as a transition between the metamorphic and igneous rock.

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