I recently examined more than 200 metamorphosed ordinary chondrites that were initially classified as unshocked or very weakly shocked because their silicate grains did not appear deformed.
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释义
我最近研究了超过200枚原来归类为未受冲击或仅受轻微冲击的普通球粒陨石,它们内部的矽酸盐矿物颗粒看来并没有变形。
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