Changes

Miyashiro (1973) in Keary and Vine (1994) states that subduction zone has paired metamorphic belts. An outher high pressure/low temperature on the seaward and low pressure/high temperature belt of similar age associated with the island arc.

Miyashiro (1973) in Keary and Vine (1994) states that subduction zone has paired metamorphic belts. An outher high pressure/low temperature on the seaward and low pressure/high temperature belt of similar age associated with the island arc.

Fig. 1. Forces in Subduction Zone (Derived and modified from Keary and Vine, 1994)

File:Subduction_Fig-1.png|Fig. 1. Forces in Subduction Zone (Derived and modified from Keary and Vine, 1994)

Fig. 2. Zonation of Deformation in Subduction Zone. This figure models the explanation above. (Derived and modified from Keary and Vine, 1994)

File:Subduction_Fig-2.png|Fig. 2. Zonation of Deformation in Subduction Zone. This figure models the explanation above. (Derived and modified from Keary and Vine, 1994)

File:Subduction_Fig-3.png|Fig. 3. Types of Subduction Zone (Derived from Jolivet and Nataf, 2001)

Fig. 3. Types of Subduction Zone (Derived from Jolivet and Nataf, 2001)

File:Subduction_Fig-4.png|Fig. 4. Structural Features of Subduction Zone (Derived from Nichols, 2009)

Fig. 4. Structural Features of Subduction Zone (Derived from Nichols, 2009)

File:Subduction_Fig-5.png|Fig. 5. Schematic Model of Island-arc (Derived from Wilson, 2007)

Fig. 5. Schematic Model of Island-arc (Derived from Wilson, 2007)

File:Subduction_Fig-6.png|Fig. 6. Plot of wt.% K2O versus wt.% SiO2 to Show Major Divisions of Island-arc Volcanic Suites (Derived from Wilson, 2007)

File:Subduction_Fig-7.png|Fig. 7. Plot of A = K2O + Na2O, F = FeO + 0,9Fe2O3, and M = MgO to Differentiate between Tholeiitic and Calc-alkaline Magma Series (Derived from Wilson, 2007)

Fig. 6. Plot of wt.% K2O versus wt.% SiO2 to Show Major Divisions of Island-arc Volcanic Suites (Derived from Wilson, 2007)

File:Subduction_Fig-8.png|Fig. 8. Schematic Model of Subduction Zone in Active Continental Margin (Derived from Winter, 2001)

Fig. 7. Plot of A = K2O + Na2O, F = FeO + 0,9Fe2O3, and M = MgO to Differentiate between Tholeiitic and Calc-alkaline Magma Series (Derived from Wilson, 2007)

File:Subduction_Fig-9.png|Fig. 9. Classification of Tectonic Settings based on Mineral Composition in Sandstone (Derived from Dickinson et. al. (1983) in Boggs (2011))

Fig. 8. Schematic Model of Subduction Zone in Active Continental Margin (Derived from Winter, 2001)

Fig. 9. Classification of Tectonic Settings based on Mineral Composition in Sandstone (Derived from Dickinson et. al. (1983) in Boggs (2011))

==References==

==References==