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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)
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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