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- W2141244066 abstract "Lunar spherules are small glass beads that are formed mainly as a result of small impacts on the lunar surface; the ages of these impacts can be determined by the (40)Ar/(39)Ar isochron technique. Here, 155 spherules separated from 1 gram of Apollo 14 soil were analyzed using this technique. The data show that over the last approximately 3.5 billion years, the cratering rate decreased by a factor of 2 to 3 to a low about 500 to 600 million years ago, then increased by a factor of 3.7 +/- 1.2 in the last 400 million years. This latter period coincided with rapid biotic evolutionary radiation on Earth." @default.
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- W2141244066 date "2000-03-10" @default.
- W2141244066 modified "2023-10-18" @default.
- W2141244066 title "Lunar Impact History from <sup>40</sup> Ar/ <sup>39</sup> Ar Dating of Glass Spherules" @default.
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- W2141244066 doi "https://doi.org/10.1126/science.287.5459.1785" @default.
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