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Deeper solar wind penetration on the Moon’s farside from noble gas records
Abstract As the Moon lacked an atmosphere and global magnetic field for much of its history, volatile elements in lunar soils are established to originate primarily from solar wind irradiation and meteorite and comet impacts. Potential differences in volatiles and their origins between the near and far sides of the Moon are not well understood. Here we report the noble gas compositions of lunar farside soils sampled by Chang’e-6.
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