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The study investigates the morphological variability of zircon crystals in the Mimoso Volcanics of Mato Grosso, Brazil, to understand their petrogenetic significance. Zircon typology reveals that these crystals formed under high temperatures and peralkaline conditions, with distinct classifications across different rock lithotypes. The findings suggest a genetic relationship between the Mimoso Volcanics and surrounding geological formations, emphasizing the role of zircon morphology in tracking magmatic evo

Author

Juan Laura

Language

EN