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The document discusses the Miocene calc-alkaline magmatism in the Apuseni Mountains, Romania, highlighting its significance in hosting large Cu-Au ore systems. It presents a model for the geotectonic evolution and melt generation processes, indicating that the magmatic activity was influenced by transtensional and rotational tectonics rather than subduction. The study emphasizes the role of fluid-present melting in the formation of mineralizing fluids and the evolution of various magma types over time.

Author

Kimik

Language

EN