Canasite, named after its discovery locality in the Cana Valley of Pakistan, is a relatively rare mineral that belongs to the silicate group. Its formation is closely linked to metamorphic processes within the Earth's crust, where intense heat and pressure transform pre-existing minerals into new crystalline structures. Typically found in association with other minerals such as calcite, quartz, and epidote, Canasite forms in metamorphic rocks, particularly in regions with significant tectonic activity.
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