抄録
Yamato-86032 is a feldspathic lunar highland meteorite, mainly composed of several types of highland lithologies. The absence of KREEP components suggests that this meteorite is derived from the farside of the Moon. We found that one light-gray feldspathic lithology contains an augite-bearing clast that is different from known highland rocks from the nearside. Coupled with the mineralogical evidence from a magnesian feldspathic lunar meteorite Dhofar 489, we suggest that the lunar farside highland crust may have experienced more variable igneous processes than previously thought.
