1887

Abstract

Summary

Geologically of Indonesia is an active magmatism path that has the potential to produce metal mineralization so that it is one of the countries that explores metal deposits. Metal mineralization is generally caused by hydrothermal activity associated with volcanic rocks. Complex hydrothermal alteration can result in changes in mineralogy, texture, and chemical content of rocks, one of which is the abundance of copper metal in the Purwoharjo area. This research was conducted to determine the distribution of Cu content in hematite minerals.

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/content/papers/10.3997/2214-4609.201977016
2019-12-02
2024-04-28
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