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This document summarizes controls on ore localization in tin-bearing veins in southwestern England. The key controls discussed are: 1. Host fracture geometry - Variations in strike and dip of fractures, and intersections and branches of veins provide dilatant zones that localize higher grades and widths of mineralization. 2. Lithology - Differences in rock types affect mechanical properties and chemical reactivity, which influence fracture shape, density, and provide zones for vein deflection/breakup rel

Author

Alvaro Madrid

Language

EN