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- W1567602646 abstract "Core 14211/10 is a 2 cm-diameter double drive tube that was collected within the smooth plains area of the Apollo 14 landing site. Rock fragments in the core appear to be derived from the smooth plains area because the coring site is beyond ejecta range of Cone Crater and is within the expected continuous ejecta of two large craters in the plains. The characteristics of the glassy soil breccia zone between 12.5 and 15.5 cm indicate that this zone represents the bottom of a glass-lined crater. At least some of the dark agglutinate and glass-rich soils at the top of the core are mature, by FMR measurements, and show maturation interrelationships between particle types. Hence, this dark interval is interpreted as a gardened zone." @default.
- W1567602646 created "2016-06-24" @default.
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- W1567602646 date "1979-01-01" @default.
- W1567602646 modified "2023-09-23" @default.
- W1567602646 title "Preliminary description and interpretation of Apollo 14 cores 14211/10" @default.
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