阿波罗
氩
样品(材料)
K–Ar测年
材料科学
地质学
化学
地球化学
生物
色谱法
动物
有机化学
作者
E. Calvin Alexander,P. K. Davis,R. S. Lewis
出处
期刊:Science
[American Association for the Advancement of Science]
日期:1972-01-28
卷期号:175 (4020): 417-419
被引量:11
标识
DOI:10.1126/science.175.4020.417
摘要
An age of 3.33+/-0.05x10(9) years was obtained for Apollo 15 sample 15555 by argon40-argon-39 dating. The age of rock 15555, a basalt from the rim of Hadley Rille, establishes an upper limit to the age of the rille. The basalt flows filling the Hadley Rille section of the Imbrium basin postdate the formation of the basin-as measured by the Apollo 14 samples of the Fra Mauro formation-by at least 500x10(6) years. Therefore, the mare basalts cannot be simple impact melts but rather must result from some igneous activity on the moon.
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