Professor Alexander Nemchin from Curtin's School of Earth and Planetary Sciences highlighted the significance of this finding, stating, "These high-magnesium glass beads may have formed when an asteroid smashed into rocks that originated from the mantle deep within the Moon. This is exciting, because we've never sampled the mantle directly before: the tiny glass beads offer us a glimpse of the Moon's hidden interior."
Co-author Professor Tim Johnson noted that these glass beads possess a unique chemistry not previously identified in surface rock samples, potentially linked to massive impacts like the formation of the Imbrium Basin, a vast crater formed over 3 billion years ago. "Remote sensing has shown the area around the basin's edge contains the kind of minerals that match the glass bead chemistry. This is a big step forward in understanding how the Moon evolved internally," Professor Johnson explained.
Lead researcher Professor Xiaolei Wang from Nanjing University emphasized the broader implications of the study, suggesting that insights into the Moon's interior could guide future robotic and crewed missions aiming to explore the Moon's deep geological layers.
Research Report:A potential mantle origin for precursor rocks of high-Mg impact glass beads in Chang'e-5 soil
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