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multiple (~300) mineral analyses show that mafic orthopyroxene (en65–80), plagioclase (an30–70), augite (wo30–45, en40–45, fs10–15), and olivine (~fo85) (in that order) represent the most abundant and commonly occurring microphenocrysts.
de multiples (~300) analyses minérales démontrent que l'orthopyroxène (en65–80), le plagioclase (an30–70), l'augite (wo30–45, en40–45, fs10–15) et l'olivine (~fo85) représentent (dans cet ordre) les microphénocristaux les plus abondants et les plus communs.
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