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- W2016303890 abstract "Abstract We report on a40Ar-39Ar study of the Apollo 16 breccia 67435 and present ages of five samples representing matrix, lithic clasts and plagioclase clasts. While the matrix age spectrum does not have a well-defined plateau, the two lithic clasts gave plateau ages of 3.96 and 4.04 AE. Since all samples had apparent ages of ∼1 AE in the fractions ≤600°C extraction temperature, the breccia might have been assembled in a rather mild process at about that time or even more recently out of material with different metamorphic ages. The two plagioclase samples, of which one was a single 9-mg mineral clast and the other a 15-mg composite of several clasts, also have ages of ∼1 AE in the low-temperature release fractions, but are apparently undisturbed by any ∼4-AE events since they both have well-defined plateaux at 4.42 AE. The age of these strongly calcic plagioclase clasts, believed to be remnants of the anorthositic lunar crust, establishes a lower age limit to the end of the early lunar differentiation and thus places a strong constraint to the lunar evolution." @default.
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- W2016303890 title "Early lunar differentiation: 4.42-AE-old plagioclase clasts in Apollo 16 breccia 67435" @default.
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- W2016303890 doi "https://doi.org/10.1016/0012-821x(78)90115-2" @default.
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