首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Calcium isotopic composition of the lunar crust, mantle, and bulk silicate Moon: A preliminary study
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Calcium isotopic composition of the lunar crust, mantle, and bulk silicate Moon: A preliminary study

机译:月球壳,地幔,散装硅酸盐月亮的钙同位素组成:初步研究

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摘要

Calcium isotopes have the potential to explore genetic links between the Moon and Earth. Here, we constrain calcium isotopic composition of the bulk silicate Moon (BSM), using petrological, geochemical and calcium isotopic data obtained from five lunar meteorites (two basalts and three feldspathic breccia rocks), and on four anorthite crystals from two feldspathic breccia meteorites. The delta Ca-44/(40) of lunar feldspathic breccias are 0.76 +/- 0.06 parts per thousand (2SD, n = 3), 0.78 +/- 0.10 parts per thousand (2SD, n = 6) and 0.82 +/- 0.02 parts per thousand (2SD, n = 3), respectively, consistent with previously determined calcium isotopic composition of feldspathic breccias. Four anorthite crystals yield a mean delta Ca-44/(40) value of 0.75 +/- 0.13 parts per thousand (2SD, n = 4), inferred to represent the Ca value of the lunar crust. The delta Ca-44/(40) values of the two lunar basalts are 0.90 +/- 0.07 parts per thousand (2SD, n = 3) and 0.96 +/- 0.11 parts per thousand (2SD, n = 4), respectively, slightly heavier than the feldspathic breccias and anorthites. The delta Ca-44/(40) of the studied lunar basalts and literature data show negative correlations with CaO, Al2O3, and anorthite mode, pointing to the effect of contamination by lunar crust rocks. Using the heaviest delta Ca-44/(40) found in the least contaminated lunar basalts and a 0.10-0.20 parts per thousand fractionation of calcium isotopes during partial melting, we estimate the delta Ca-44/(40) value of the lunar mantle to be 0.96-1.11 parts per thousand. The delta Ca-44/(40) values of the BSM is estimated to be 0.89-0.95 parts per thousand, using a two-end member mixing model. The Ca isotopic composition of the BSM is within error to that of the bulk silicate Earth (0.94 +/- 0.05 parts per thousand), providing insights into the information of the comparison of the Earth-Moon system and the planets of inner Solar System. (C) 2019 Elsevier Ltd. All rights reserved.
机译:钙同位素有可能探索月球和地球之间的遗传联系。在这里,我们限制了来自五个月球陨石(两个沼泽和三种股骨岩石岩)的岩石,地球化学和同位素数据,以及来自两个长期性的Breccia陨石的四个钙质晶体的肉质,地球化学和钙同位素数据的钙同位素组合物。 Lunar FeldPhathic Breccias的Delta Ca-44 /(40)为0.76 +/- 0.06份(2SD,N = 3),0.78 +/- 0.10份(2SD,N = 6)和0.82 +/-分别为0.02份(2SD,N = 3),与先前确定的钙磷酸钙组合物一致。四个钙质晶体产生平均delta ca-44 /(40)值0.75 +/- 0.13份/份每千份(2SD,N = 4),推断出代表月球地壳的Ca值。两个月球基础的Delta Ca-44 /(40)值分别为0.90 +/- 0.07份(2SD,N = 3)和0.96 +/- 0.11分别,分别为每千(2SD,N = 4),比长期性的飞行粘性和钙质略重。学习的月球基础和文献数据的Delta CA-44 /(40)显示了与CAO,AL2O3和钙抗石模式的负相关,指向月球地壳岩石的污染效果。使用最少污染的月球玄武岩中的最重的ΔCa-44 /(40)和部分熔化期间每千钙同位素的0.10-0.20份分馏,我们估计了月球地幔的Delta Ca-44 /(40)的价值每千份0.96-1.11份。使用双端成员混合模型,BSM的Delta Ca-44 /(40)值估计为0.89-0.95份。 BSM的Ca同位素组合物在散装硅酸盐地球(0.94 +/- 0.05份)的误差内,提供了进入地球系统和内阳系统行星的信息的见解。 (c)2019年elestvier有限公司保留所有权利。

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