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The dissertation by Sandra M. Hamaker explores the relationship between fault zone architecture and groundwater compartmentalization in the East Tintic Mining District, Utah. It focuses on the Eureka Lilly fault zone, which acts as an impermeable barrier for groundwater flow, separating distinct groundwater systems with varying temperatures and compositions. The study highlights how the fault's damage zone contains interconnected fractures that facilitate groundwater movement, while the fault core is characterized by impermeable breccia that compartmentalizes these water sources. The findings challenge traditional concepts of basin flow and emphasize the complexity of groundwater dynamics influenced by geological structures.

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