• 文献检索
  • 文档翻译
  • 深度研究
  • 学术资讯
  • Suppr Zotero 插件Zotero 插件
  • 邀请有礼
  • 套餐&价格
  • 历史记录
应用&插件
Suppr Zotero 插件Zotero 插件浏览器插件Mac 客户端Windows 客户端微信小程序
定价
高级版会员购买积分包购买API积分包
服务
文献检索文档翻译深度研究API 文档MCP 服务
关于我们
关于 Suppr公司介绍联系我们用户协议隐私条款
关注我们

Suppr 超能文献

核心技术专利:CN118964589B侵权必究
粤ICP备2023148730 号-1Suppr @ 2026

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验

寻找暴露在月球表面的月幔岩石。

The search for lunar mantle rocks exposed on the surface of the Moon.

作者信息

Moriarty Daniel P, Dygert Nick, Valencia Sarah N, Watkins Ryan N, Petro Noah E

机构信息

NASA Goddard Space Flight Center, Greenbelt, MD, USA.

University of Maryland, College Park, MD, USA.

出版信息

Nat Commun. 2021 Aug 3;12(1):4659. doi: 10.1038/s41467-021-24626-3.

DOI:10.1038/s41467-021-24626-3
PMID:34344883
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8333336/
Abstract

The lunar surface is ancient and well-preserved, recording Solar System history and planetary evolution processes. Ancient basin-scale impacts excavated lunar mantle rocks, which are expected to remain present on the surface. Sampling these rocks would provide insight into fundamental planetary processes, including differentiation and magmatic evolution. There is contention among lunar scientists as to what lithologies make up the upper lunar mantle, and where they may have been exposed on the surface. We review dynamical models of lunar differentiation in the context of recent experiments and spacecraft data, assessing candidate lithologies, their distribution, and implications for lunar evolution.

摘要

月球表面古老且保存完好,记录着太阳系历史和行星演化过程。古代盆地规模的撞击挖掘出了月球地幔岩石,预计这些岩石仍存在于月球表面。采集这些岩石样本将有助于深入了解包括分化和岩浆演化在内的基本行星过程。月球科学家们对于构成月球上地幔的岩性以及它们可能在月球表面何处暴露存在争议。我们结合近期实验和航天器数据,对月球分化的动力学模型进行综述,评估候选岩性、它们的分布以及对月球演化的影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a510/8333336/37ac84d105d8/41467_2021_24626_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a510/8333336/09b5415aee7d/41467_2021_24626_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a510/8333336/ae0306086503/41467_2021_24626_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a510/8333336/37ac84d105d8/41467_2021_24626_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a510/8333336/09b5415aee7d/41467_2021_24626_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a510/8333336/ae0306086503/41467_2021_24626_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a510/8333336/37ac84d105d8/41467_2021_24626_Fig3_HTML.jpg

相似文献

1
The search for lunar mantle rocks exposed on the surface of the Moon.寻找暴露在月球表面的月幔岩石。
Nat Commun. 2021 Aug 3;12(1):4659. doi: 10.1038/s41467-021-24626-3.
2
Of time and the moon.关于时间和月亮。
Science. 1971 Jul 30;173(3995):383-92. doi: 10.1126/science.173.3995.383.
3
The Evolution of a Spacecraft-Generated Lunar Exosphere.航天器产生的月球外逸层的演变
J Geophys Res Planets. 2020 Aug;125(8). doi: 10.1029/2020je006464. Epub 2020 Aug 11.
4
Magnesium stable isotopes support the lunar magma ocean cumulate remelting model for mare basalts.镁稳定同位素支持月幔岩浆洋结晶堆积再熔融模型解释月海玄武岩成因。
Proc Natl Acad Sci U S A. 2019 Jan 2;116(1):73-78. doi: 10.1073/pnas.1811377115. Epub 2018 Dec 17.
5
Late formation and prolonged differentiation of the Moon inferred from W isotopes in lunar metals.根据月球金属中的钨同位素推断月球的晚期形成与长期分化。
Nature. 2007 Dec 20;450(7173):1206-9. doi: 10.1038/nature06428.
6
Scientific investigations at a lunar base.在月球基地进行的科学调查。
Acta Astronaut. 1988 Jul;17(7):675-90. doi: 10.1016/0094-5765(88)90183-x.
7
Geological context of the Chang'e-6 landing area and implications for sample analysis.嫦娥六号着陆区的地质背景及其对样品分析的意义。
Innovation (Camb). 2024 Jun 24;5(5):100663. doi: 10.1016/j.xinn.2024.100663. eCollection 2024 Sep 9.
8
Chang'E-4 initial spectroscopic identification of lunar far-side mantle-derived materials.嫦娥四号对月球远侧幔源物质的初始光谱识别。
Nature. 2019 May;569(7756):378-382. doi: 10.1038/s41586-019-1189-0. Epub 2019 May 15.
9
Zinc isotopic evidence for the origin of the Moon.锌同位素证据表明月球的起源。
Nature. 2012 Oct 18;490(7420):376-9. doi: 10.1038/nature11507.
10
Petrologic Characteristics of the Lunar Surface.月球表面的岩石学特征。
Sci Rep. 2015 Nov 27;5:17075. doi: 10.1038/srep17075.

引用本文的文献

1
A potential mantle origin for precursor rocks of high-Mg impact glass beads in Chang'e-5 soil.嫦娥五号月壤中高镁撞击玻璃珠前驱体岩石的潜在地幔起源
Sci Adv. 2025 May 9;11(19):eadv9019. doi: 10.1126/sciadv.adv9019.
2
Lunar primitive mantle olivine returned by Chang'e-6.嫦娥六号带回的月表原始地幔橄榄石。
Nat Commun. 2025 Apr 23;16(1):3759. doi: 10.1038/s41467-025-58820-4.
3
Oxygen isotope identity of the Earth and Moon with implications for the formation of the Moon and source of volatiles.地球与月球的氧同位素特征及其对月球形成和挥发性物质来源的启示

本文引用的文献

1
Impact Melt Facies in the Moon's Crisium Basin: Identifying, Characterizing, and Future Radiogenic Dating.月球危海盆地中的撞击熔体相:识别、表征及未来放射性定年
J Geophys Res Planets. 2020 Jan;125(1):e2019JE006024. doi: 10.1029/2019JE006024. Epub 2020 Jan 5.
2
A long-lived magma ocean on a young Moon.年轻月球上的长寿岩浆海洋。
Sci Adv. 2020 Jul 10;6(28):eaba8949. doi: 10.1126/sciadv.aba8949. eCollection 2020 Jul.
3
Chang'E-4 initial spectroscopic identification of lunar far-side mantle-derived materials.嫦娥四号对月球远侧幔源物质的初始光谱识别。
Proc Natl Acad Sci U S A. 2024 Dec 24;121(52):e2321070121. doi: 10.1073/pnas.2321070121. Epub 2024 Dec 16.
4
Nature of the lunar far-side samples returned by the Chang'E-6 mission.嫦娥六号任务带回的月球背面样本的性质。
Natl Sci Rev. 2024 Sep 16;11(11):nwae328. doi: 10.1093/nsr/nwae328. eCollection 2024 Nov.
5
Lunar rock investigation and tri-aspect characterization of lunar farside regolith by a digital twin.通过数字孪生对月球背面风化层进行月球岩石研究和三方面表征。
Nat Commun. 2024 Mar 8;15(1):2098. doi: 10.1038/s41467-024-46233-8.
6
Rapid transition from primary to secondary crust building on the Moon explained by mantle overturn.地幔翻转解释了月球上从原始地壳到次生地壳的快速转变。
Nat Commun. 2023 Aug 17;14(1):5002. doi: 10.1038/s41467-023-40751-7.
7
A changing thermal regime revealed from shallow to deep basalt source melting in the Moon.月球浅层至深层玄武岩源区熔融所揭示的热状态变化
Nat Commun. 2022 Dec 9;13(1):7594. doi: 10.1038/s41467-022-35260-y.
8
A lunar sample renaissance.月球样本复兴。
Nat Commun. 2021 Dec 14;12(1):7053. doi: 10.1038/s41467-021-27296-3.
Nature. 2019 May;569(7756):378-382. doi: 10.1038/s41586-019-1189-0. Epub 2019 May 15.
4
Structure and evolution of the lunar Procellarum region as revealed by GRAIL gravity data.月球 Procellarum 区域的结构和演化,由 GRAIL 重力数据揭示。
Nature. 2014 Oct 2;514(7520):68-71. doi: 10.1038/nature13697.
5
The crust of the Moon as seen by GRAIL.月球的地壳——GRAIL 的观测结果。
Science. 2013 Feb 8;339(6120):671-5. doi: 10.1126/science.1231530. Epub 2012 Dec 5.
6
Chronological evidence that the Moon is either young or did not have a global magma ocean.月球要么很年轻,要么没有全球性岩浆海洋的年代证据。
Nature. 2011 Aug 17;477(7362):70-2. doi: 10.1038/nature10328.
7
Evidence of a global magma ocean in Io's interior.木卫一内部存在全球岩浆海洋的证据。
Science. 2011 Jun 3;332(6034):1186-9. doi: 10.1126/science.1201425. Epub 2011 May 12.
8
Detection of water in the LCROSS ejecta plume.探测 LCROSS 喷射羽流中的水。
Science. 2010 Oct 22;330(6003):463-8. doi: 10.1126/science.1186986.
9
Volatile content of lunar volcanic glasses and the presence of water in the Moon's interior.月球火山玻璃的挥发性成分与月球内部水的存在
Nature. 2008 Jul 10;454(7201):192-5. doi: 10.1038/nature07047.
10
Lunar anorthosites: rare-Earth and other elemental abundances.月球斜长岩:稀土元素和其他元素的丰度。
Science. 1970 Nov 27;170(3961):969-74. doi: 10.1126/science.170.3961.969.