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Explore the transformative process of metamorphism on existing rocks due to different conditions, such as heat, pressure, and fluids. Learn about types of metamorphism, agents, textures, and common metamorphic rocks like slate and gneiss.
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Metamorphism and metamorphic Rocks Prof. Dr. Ziad Salem Abu-Hamatteh Faculty of Engineering Technology Al-Balqa’ Applied University
Metamorphism and metamorphic Rocks Metamorphism: all changes (textural/mineralogical) that take place on a pre-existing rock(I,S,M) in response to new conditions (P/T) imposed on the rock which are different from those under which the rocks have originally been formed. Changes take place in the solid state
Original Unmetamorphosed rock A B Nucleation of new minerals in response to changes in T or P or both Ions migrate either by solid state diffusion or Different stages of mineral growth involve both textural and mineralogical changes Intergranular fluids C SiO2 + CaCO3 CaSiO3 + CO2 Best, 1982
Types or Envs. of metamorphism • Contact (thermal) metamorphism = around magmas • Regional metamorphism = along subduction zones in areas of mountain building. Rocks in these setting are subjected to both increase in T and to directed pressures.
Agents of metamorphism • Heat = thermal energy geothermal gradient • Pressure increases at a rate of about 250-300 bars/km of depth. • Chemical active hot fluids (H2O, CO2 are the most common) moving within the rocks are capable of dissolving rocks and precipitating others at other places
Textures • Foliated rocks • = regional • Metamorphic • rocks
Phyllite http://geology.about.com/library/bl/images/blphyllite.htm