Milky Quartz Veins in Amphibolite
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Quartz deposits are often found within amphibolite rock formations, which comprise metamorphic minerals such as hornblende and garnet. These quartz deposits frequently exhibit well-defined vein structures that cut through the surrounding amphibolite. The presence of quartz veins within amphibolite can be indicative of fluid movement and mineralization processes during high-grade metamorphism.
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