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This document summarizes a study on the primary tin deposit in the Airdibi area of Bangka Island, Indonesia. The researchers conducted geological mapping and laboratory analysis to characterize the deposit. They identified six alteration mineral assemblage zones formed by hydrothermal processes. Mineralization occurred along joints and faults filled with minerals like tourmaline and silica. Analysis found cassiterite and other ore minerals associated with tourmaline, quartz, and granite dykes. Tin content v

Author

Saifullah Fatah

Language

EN