Potential epithermal feeder structure
A potential epithermal feeder structure refers to the subsurface geological feature through which hydrothermal fluids, rich in precious metals like gold and silver, ascend from depth to form epithermal deposits. These structures are crucial for localizing mineralization and are characterized by steep dips and linear traces, often coinciding with faults or fractures that act as pathways for the mineralizing fluids. Exploration geologists look for these structures to identify potential areas of economic mineralization within epithermal systems
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