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This document discusses the discovery of a Middle Ordovician metagranitoid in the Anatolide-Tauride Block of northwest Turkey, providing evidence for Ordovician magmatism in the region. The metagranitoid, characterized by specific geochemical properties, is suggested to be a remnant of the crystalline basement and underwent high-pressure metamorphism during the Late Cretaceous. Zircon dating indicates a crystallization age of approximately 467 Ma, linking it to the geological history of the northern margin

Author

mehmethanatasoy

Language

EN