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The calc-alkaline magma series is a major type of igneous rock formation characterized by a range of volcanic and intrusive rock types, including basalt and granite. These rocks are distinguished from tholeiitic magmas by their oxidized state and consistent iron content during crystallization. Calc-alkaline rocks are typically found in volcanic arcs above subduction zones and are believed to form through processes such as fractional crystallization and interaction with subducted materials.

Author

NiaziBashir

Language

EN