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This thesis examines the structural architecture and geological framework of the Buriticá gold deposit in Colombia. The deposit is hosted within a Miocene-aged intrusive complex located in the Middle Cauca belt. The deposit formed as a fault-controlled hydrothermal system along long-lived penetrative faults that provided pathways for fluid flow and multiple stages of vein formation. Sericite alteration controls the distribution of gold grades in the Yaraguá and Veta Sur mineralized systems. Lithogeochemical

Author
Cristina Dallos
Language
EN