Geochronology of high-K aluminous mare basalt clasts from Apollo 14 breccia 14304

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Abundance, Basalt, Geochronology, Igneous Rocks, Lunar Maria, Apollo 14 Flight, Magma, Moon, Chronology, Potassium, Aluminum, Basalts, Maria, Clasts, Breccias, Apollo 14, 14303, Age, Isotopic Ratios, Petrogenesis, Isochron Ages, Source, Origin, Fractionation, Enrichment, Sample, Lunar, Experiments, Laboratory Studies, Procedure, Rubidium, Strontium, Samarium, Neodymium, Potassium, Lanthanum, Abundance

Scientific paper

Two aluminous mare basalt clasts of high K abundances from Apollo 14 breccia 14304 (the 14304,127 and 14304,128 samples) were characterized with respect to the Rb and Sr concentrations and isotopic compositions, and the Rb-Sr, K-Ar, and Sm-Nd isotopic age determinations were carried out. The results suggest that these high-K basalts were melts derived from mantle material and that they have experienced about ten-fold Rb/Sr and K/La enrichments at approximately the time of crystallization.

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