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The article presents a metallogenic model for the Eocene Santa María and Antares Zn-Pb(Ag) skarn deposits in the Velardeña Mining District of Durango, Mexico, detailing their formation stages and mineralogical characteristics. It describes the evolution of these deposits through prograde, retrograde, post-ore, and late stages influenced by varying fluid temperatures and compositions. The study utilizes petrography, fluid inclusion analysis, stable isotopes, and geochronology to provide insights into the gen

Author

posiyev364

Language

EN