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- W2000207708 abstract "A Rb-Sr internal isochron on a 62 mg basaltic boulder from the Luna 16 mission yields an age of 3.42 ± 0.18 AE and a low initial87Sr/86Sr 0.69906 ∓ 4 (1σ errors). The total range in measured87Sr/86Sr for mineral separates of this sample was 1.3 per mil. The ages of basalts from four mare sites determine a narrow time interval of 0.55 AE for the flooding of the maria. Initial87Sr/86Sr for these basalts are restricted to extremely low values, indicating that they all originated in low Rb/Sr regions. Luna 16 soils have low Rb/Sr (≈ 0.007) and yield model ages TBABI = 4.2 ± 0.3AE and TBABI = 4.1 ± 0.3AE. Lunar soils from Apollo 11, 12, 14, 15 and Luna 16 all lie very close to a 4.6 AE isochron which passes through BABI. This appears to be a universal characteristic of lunar soils and must correspond to lunar differentiation processes closely following the time of formation of the moon." @default.
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- W2000207708 title "Rb‐Sr age of a Luna 16 basalt and the model age of lunar soils" @default.
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