Komatiitic parental magmas of the Archean Ujaragssuit Nunât ultramafic body, SW Greenland, identified from spinel chemistry

IF 3.5 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
I. Nishio, T. Morishita, P. Waterton, A. Tamura, K. Itano, S. H. Serre, J. L. Plesner, K. Takahashi, K. Tani, Y. Harigane, H. Sawada, K. Szilas
{"title":"Komatiitic parental magmas of the Archean Ujaragssuit Nunât ultramafic body, SW Greenland, identified from spinel chemistry","authors":"I. Nishio,&nbsp;T. Morishita,&nbsp;P. Waterton,&nbsp;A. Tamura,&nbsp;K. Itano,&nbsp;S. H. Serre,&nbsp;J. L. Plesner,&nbsp;K. Takahashi,&nbsp;K. Tani,&nbsp;Y. Harigane,&nbsp;H. Sawada,&nbsp;K. Szilas","doi":"10.1007/s00410-025-02208-6","DOIUrl":null,"url":null,"abstract":"<div><p>Archean and Proterozoic layered intrusions represent an important portion of the igneous rock archive and their parental magma composition may provide crucial insights into the Earth’s magmatic and geodynamic evolution. Both komatiitic and boninitic parental magmas have been suggested for several major Archean layered intrusions, which could imply different tectonic settings for their formation. We studied the ~ 3.2 Ga Ujaragssuit Nunât layered ultramafic body from southern West Greenland (Ujaragssuit ultramafic body), which contains some of Earth’s oldest chromitites. Spinel major and trace elements, and whole-rock platinum group element compositions in massive chromitites from the Ujaragssuit ultramafic body, largely preserve primary igneous compositions. In contrast, spinels from most silicate-dominated ultramafic rocks were altered by metamorphic and metasomatic events. We collated a large spinel dataset to investigate variations in their parental magma compositions and tectonic settings using multivariate statistical analysis. Both the massive chromitites from the Ujaragssuit ultramafic body and chromitites from other Archean and Proterozoic ultramafic layered intrusion show high Cr/(Cr + Al) and Ti/V ratios in spinel, and high whole-rock Ir and Ru contents, which are consistent with those of komatiitic spinel. The compositions of chromitites suggest that the parental magmas of the Ujaragssuit ultramafic body are komatiitic, implying that the formation of these layered intrusions was related to mantle plumes. Our recognition of a komatiitic ultramafic body in North Atlantic Craton, where no komatiite has previously been reported, suggests that komatiitic magmas were a common feature among cratons.</p></div>","PeriodicalId":526,"journal":{"name":"Contributions to Mineralogy and Petrology","volume":"180 3","pages":""},"PeriodicalIF":3.5000,"publicationDate":"2025-02-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s00410-025-02208-6.pdf","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Contributions to Mineralogy and Petrology","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1007/s00410-025-02208-6","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0

Abstract

Archean and Proterozoic layered intrusions represent an important portion of the igneous rock archive and their parental magma composition may provide crucial insights into the Earth’s magmatic and geodynamic evolution. Both komatiitic and boninitic parental magmas have been suggested for several major Archean layered intrusions, which could imply different tectonic settings for their formation. We studied the ~ 3.2 Ga Ujaragssuit Nunât layered ultramafic body from southern West Greenland (Ujaragssuit ultramafic body), which contains some of Earth’s oldest chromitites. Spinel major and trace elements, and whole-rock platinum group element compositions in massive chromitites from the Ujaragssuit ultramafic body, largely preserve primary igneous compositions. In contrast, spinels from most silicate-dominated ultramafic rocks were altered by metamorphic and metasomatic events. We collated a large spinel dataset to investigate variations in their parental magma compositions and tectonic settings using multivariate statistical analysis. Both the massive chromitites from the Ujaragssuit ultramafic body and chromitites from other Archean and Proterozoic ultramafic layered intrusion show high Cr/(Cr + Al) and Ti/V ratios in spinel, and high whole-rock Ir and Ru contents, which are consistent with those of komatiitic spinel. The compositions of chromitites suggest that the parental magmas of the Ujaragssuit ultramafic body are komatiitic, implying that the formation of these layered intrusions was related to mantle plumes. Our recognition of a komatiitic ultramafic body in North Atlantic Craton, where no komatiite has previously been reported, suggests that komatiitic magmas were a common feature among cratons.

格陵兰西南部太古宙Ujaragssuit nun超镁铁质体科马提岩母岩浆的尖晶石化学鉴定
太古宙和元古代的层状侵入岩是火成岩档案的重要组成部分,它们的母岩浆组成可以为了解地球岩浆和地球动力学演化提供重要的信息。在几次太古宙主要的层状侵入岩中,均发现了马马岩质和波长岩质的母岩浆,这可能暗示了它们形成的不同构造背景。我们研究了西格陵兰岛南部~ 3.2 Ga Ujaragssuit nun层状超镁铁质体(Ujaragssuit超镁铁质体),其中含有一些地球上最古老的铬铁矿。乌jaragssuit超基性体块状铬铁矿中尖晶石主微量元素和全岩铂族元素组成基本保持了原生火成岩组成。而绝大多数硅酸盐为主的超镁铁质岩石的尖晶石则受到变质和交代作用的蚀变。我们整理了一个大型尖晶石数据集,利用多元统计分析研究了它们的母岩浆成分和构造环境的变化。Ujaragssuit超基性岩体的块状铬铁矿和其他太古宙和元古代超基性层状侵入体的铬铁矿均表现出高Cr/(Cr + Al)和Ti/V比值,以及高的全岩Ir和Ru含量,与科马马质尖晶石一致。铬铁矿组成表明,乌jaragssuit超基性岩体的母岩浆为马马岩质岩浆,暗示这些层状侵入体的形成与地幔柱有关。我们在北大西洋克拉通中发现了一个科马提岩超镁铁质体,而以前没有报道过科马提岩,这表明科马提岩岩浆是克拉通的共同特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Contributions to Mineralogy and Petrology
Contributions to Mineralogy and Petrology 地学-地球化学与地球物理
CiteScore
6.50
自引率
5.70%
发文量
94
审稿时长
1.7 months
期刊介绍: Contributions to Mineralogy and Petrology is an international journal that accepts high quality research papers in the fields of igneous and metamorphic petrology, geochemistry and mineralogy. Topics of interest include: major element, trace element and isotope geochemistry, geochronology, experimental petrology, igneous and metamorphic petrology, mineralogy, major and trace element mineral chemistry and thermodynamic modeling of petrologic and geochemical processes.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信