Crystallization Conditions and Petrogenetic Characterization of Metaluminous to Peraluminous Calc-Alkaline Orogenic Granitoids from Mineralogical Systematics: The Case of the Cambr... by Priscila S. Zandomeni, Juan A. Moreno, Sebastián O. Verdecchia, Edgardo G. Baldo, Juan A. Dahlquist, Matías M. Morales Cámera, Catalina Balbis, Manuela Benítez, Samanta Serra-Varela, Carlos I. Lembo Wuest

“…The Sierra de Guasayán (Eastern Sierras Pampeanas, Argentina) is formed by low to medium grade metamorphic rocks intruded by Cambrian metaluminous (La Soledad quartz-diorite), slightly peraluminous (Guasayán, El Escondido and El Martirizado granodiorite plutons), and strongly peraluminous (Alto Bello granodiorite) granitoids of the Pampean magmatic arc. …”
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