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DOI | 10.1073/pnas.1811377115 |
Magnesium stable isotopes support the lunar magma ocean cumulate remelting model for mare basalts | |
Sedaghatpour, Fatemeh; Jacobsen, Stein B. | |
2019 | |
发表期刊 | PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA |
ISSN | 0027-8424 |
出版年 | 2019 |
卷号 | 116期号:1页码:73-78 |
文章类型 | Article |
语种 | 英语 |
国家 | USA |
英文摘要 | We report high-precision Mg isotopic analyses of different types of lunar samples including two pristine Mg-suite rocks (72415 and 76535), basalts, anorthosites, breccias, mineral separates, and lunar meteorites. The Mg isotopic composition of the dunite 72415 (delta Mg-25 = -0.140 +/- 0.010%, delta Mg-26 = -0.291 +/- 0.018%), the most Mg-rich and possibly the oldest lunar sample, may provide the best estimate of the Mg isotopic composition of the bulk silicate Moon (BSM). This delta Mg-26 value of the Moon is similar to those of the Earth and chondrites and reflects both the relative homogeneity of Mg isotopes in the solar system and the lack of Mg isotope fractionation by the Moon-forming giant impact. In contrast to the behavior of Mg isotopes in terrestrial basalts and mantle rocks, Mg isotopic data on lunar samples show isotopic variations among the basalts and pristine anorthositic rocks reflecting isotopic fractionation during the early lunar magma ocean (LMO) differentiation. Calculated evolutions of delta Mg-26 values during the LMO differentiation are consistent with the observed delta Mg-26 variations in lunar samples, implying that Mg isotope variations in lunar basalts are consistent with their origin by remelting of distinct LMO cumulates. |
英文关键词 | magnesium isotopes the Moon magmatic differentiation isotope fractionation lunar basalts |
领域 | 地球科学 ; 气候变化 ; 资源环境 |
收录类别 | SCI-E |
WOS记录号 | WOS:000454707700016 |
WOS关键词 | FRACTIONAL CRYSTALLIZATION ; IRON ; ORIGIN ; EARTH ; TITANIUM ; MOON ; GEOCHEMISTRY ; CONSTRAINTS ; PETROLOGY ; OXYGEN |
WOS类目 | Multidisciplinary Sciences |
WOS研究方向 | Science & Technology - Other Topics |
URL | 查看原文 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/205057 |
专题 | 地球科学 资源环境科学 气候变化 |
作者单位 | Harvard Univ, Dept Earth & Planetary Sci, 20 Oxford St, Cambridge, MA 02138 USA |
推荐引用方式 GB/T 7714 | Sedaghatpour, Fatemeh,Jacobsen, Stein B.. Magnesium stable isotopes support the lunar magma ocean cumulate remelting model for mare basalts[J]. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA,2019,116(1):73-78. |
APA | Sedaghatpour, Fatemeh,&Jacobsen, Stein B..(2019).Magnesium stable isotopes support the lunar magma ocean cumulate remelting model for mare basalts.PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA,116(1),73-78. |
MLA | Sedaghatpour, Fatemeh,et al."Magnesium stable isotopes support the lunar magma ocean cumulate remelting model for mare basalts".PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA 116.1(2019):73-78. |
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