Answer:✨❤️
Most (~80%) of the Parícutin magma is basaltic andesite with 2–3% phenocrystic olivine and microphenocrysts (and microlites) of plagioclase, olivine, orthopyroxene and clinopyroxene (Wilcox, 1954). Early (February 22, 1943) and late (1950, 1952) lavas also contain minor phenocrystic plagioclase
Explanation:
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