Probable age of Autolycus and calibration of lunar stratigraphy

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Moon, Stratigraphy, Age Dating, Argon, Isotopes, Samples, Lunar, Kreep, Apollo 15 Mission, Basalt, Impact Effects, Shock Effects, Autolycus, Laboratory Studies, 15434, Isotopic Ratios, Craters, 15358, Age, Flux

Scientific paper

Ar-39 - Ar-40 analyses of three petrographically distinct, shocked Apollo 15 KREEP (i.e., high K, rare earth element, P, and other trace element contents) basalt samples demonstrate that a major impact event affected all three samples at about 2.1 Ga. The Copernican System craters Aristillus and Autolycus are to the north. Autolycus, the older of the two, is in a particularly appropriate terrain and is the most likely source of the 2.1 Ga heating and delivery event. With this calibration point, and if Autolycus really is a Copernican crater, the Copernican System lasted twice as long as has previously been suggested. Furthermore, the moon was not subjected to a constant cratering rate over the past 3 billion years; the average rate in the preceding Eratosthenian must have been twice that in the Copernican.

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