Crystallization Conditions and PetrogeneticCharacterization of Metaluminous to PeraluminousCalc-Alkaline Orogenic Granitoids from MineralogicalSystematics: The Case of the Cambrian Magmatism from the Sierra de Guasayán (Argentina)

Crystallization Conditions and PetrogeneticCharacterization of Metaluminous to PeraluminousCalc-Alkaline Orogenic Granitoids from MineralogicalSystematics: The Case of the Cambrian Magmatism from the Sierra de Guasayán (Argentina)

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 Bell...

Full description

Bibliographic Details
Main Authors: 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
Format: Article
Language:English
Published: MDPI AG 2021-02-01
Series:Minerals
Subjects:
I-type granitoids
S-type granitoids
hybrid granitoids
mineral chemistry
geothermobarometry
Sierra de Guasayán
Online Access:https://www.mdpi.com/2075-163X/11/2/166

Internet

https://www.mdpi.com/2075-163X/11/2/166

Similar Items