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- W1996015385 abstract "Chemical data (28 major, minor, and trace elements) were obtained by instrumental neutron activation analysis (INAA) for 38 hand-picked highland fragments (1–20 mg) from coarse fines 10085. The Apollo 11 highland chemical groups are represented by a range of petrographic types. Six major chemical highland groups are identified in the Apollo 11 fragments. These are (1) high-K KREEP; (2) anorthosite (e.g., 15415, 60015) with 10× chondrite rare-earth-elements (REE) abundances, a positive Eu anomaly, anorthosite with 30× chondrite abundances, and a positive Eu anomaly; (3) anorthosite-norite-troctolite (ANT) (67075); (4) Low-K Fra Mauro (LKFM) (77135); (5) anorthositic gabbro (68415) with no Eu anomaly, anorthositic gabbro (65055, 67955) with a positive Eu anomaly, and anorthositic gabbro (68516, 60015) with a negative Eu anomaly; and (6) Apollo 11 ‘dominant highland component,’ 2×–10× chondrite REE abundances with a positive 10×–14× chondrite Eu anomaly. There are three newly-recognized groups in the Apollo 11 highland suite, based on the REE patterns. These are: (a) ANT with 5× chondrite La, 22× chondrite abundances, and a positive Eu anomaly; (b) 10× chondrite flat pattern with 14× chondrite positive Eu anomaly; and (c) 2–3× chondrite flat pattern with 10× chondrite positive Eu anomaly. The Apollo 11 highland suite is very low in potassium (non-KREEPy). Overall, the Apollo 11 highland suite is quite similar to the Apollo 16 suite. Most previously recognized highland chemical groups are represented in the Apollo 11 highland component." @default.
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- W1996015385 date "1983-01-01" @default.
- W1996015385 modified "2023-09-30" @default.
- W1996015385 title "Chemistry of the Apollo 11 Highland Component" @default.
- W1996015385 cites W1969247452 @default.
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- W1996015385 doi "https://doi.org/10.1029/jb088is01p0b139" @default.
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