Technical note: Rapid phase identification of apatite and zircon grains for geochronology using X-ray micro-computed tomography

IF 2.7 Q2 GEOCHEMISTRY & GEOPHYSICS
E. Cooperdock, F. Hofmann, Ryley M. C. Tibbetts, Anahi Carrera, Aya Takase, A. Celestian
{"title":"Technical note: Rapid phase identification of apatite and zircon grains for geochronology using X-ray micro-computed tomography","authors":"E. Cooperdock, F. Hofmann, Ryley M. C. Tibbetts, Anahi Carrera, Aya Takase, A. Celestian","doi":"10.5194/gchron-4-501-2022","DOIUrl":null,"url":null,"abstract":"Abstract. Apatite and zircon are among the best-studied and most widely used accessory\nminerals for geochronology and thermochronology. Given that apatite and\nzircon are often present in the same lithologies, distinguishing the two\nphases in crushed mineral separates is a common task for geochronology,\nthermochronology, and petrochronology studies. Here we present a method for\nefficient and accurate apatite and zircon mineral phase identification and\nverification using X-ray micro-computed tomography (microCT) of grain mounts\nthat provides additional three-dimensional grain size, shape, and inclusion\nsuite information. In this study, we analyze apatite and zircon grains from\nFish Canyon Tuff samples that went through methylene iodide (MEI) and lithium\nheteropolytungstate (LST) heavy liquid density separations. We validate the\nmicroCT results using known standards and phase identification with Raman\nspectroscopy, demonstrating that apatite and zircon are distinguishable from\neach other and other common phases, e.g., titanite, based on microCT X-ray\ndensity. We present recommended microCT scanning protocols after\nsystematically testing the effects of different scanning parameters and\nsample positions. This methodology can help to reduce time spent performing\ndensity separations with highly toxic chemicals and visually inspecting\ngrains under a light microscope, and the improved mineral identification and\ncharacterization can make geochronologic data more robust.\n","PeriodicalId":12723,"journal":{"name":"Geochronology","volume":"163 1","pages":""},"PeriodicalIF":2.7000,"publicationDate":"2022-07-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geochronology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5194/gchron-4-501-2022","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 2

Abstract

Abstract. Apatite and zircon are among the best-studied and most widely used accessory minerals for geochronology and thermochronology. Given that apatite and zircon are often present in the same lithologies, distinguishing the two phases in crushed mineral separates is a common task for geochronology, thermochronology, and petrochronology studies. Here we present a method for efficient and accurate apatite and zircon mineral phase identification and verification using X-ray micro-computed tomography (microCT) of grain mounts that provides additional three-dimensional grain size, shape, and inclusion suite information. In this study, we analyze apatite and zircon grains from Fish Canyon Tuff samples that went through methylene iodide (MEI) and lithium heteropolytungstate (LST) heavy liquid density separations. We validate the microCT results using known standards and phase identification with Raman spectroscopy, demonstrating that apatite and zircon are distinguishable from each other and other common phases, e.g., titanite, based on microCT X-ray density. We present recommended microCT scanning protocols after systematically testing the effects of different scanning parameters and sample positions. This methodology can help to reduce time spent performing density separations with highly toxic chemicals and visually inspecting grains under a light microscope, and the improved mineral identification and characterization can make geochronologic data more robust.
技术说明:用于地质年代学的磷灰石和锆石颗粒的x射线显微计算机断层扫描快速相鉴别
摘要磷灰石和锆石是地球年代学和热年代学中研究得最好、应用最广泛的辅助矿物。考虑到磷灰石和锆石经常出现在相同的岩性中,区分破碎矿物分离中的两相是地质年代学、热年代学和岩石年代学研究的共同任务。在这里,我们提出了一种高效、准确的磷灰石和锆石矿物相识别和验证方法,该方法使用颗粒丘的x射线微计算机断层扫描(microCT),提供额外的三维颗粒尺寸、形状和包裹体信息。本研究对鱼谷凝灰岩样品中磷灰石和锆石颗粒进行了亚碘化甲烷(MEI)和锂杂多钨酸盐(LST)重液密度分离。我们使用已知的标准和拉曼光谱相识别验证了microCT结果,证明了磷灰石和锆石是相互区分的,以及其他常见的相,例如钛矿,基于microCT x射线密度。在系统测试了不同扫描参数和样品位置的影响后,我们提出了推荐的微ct扫描方案。这种方法可以帮助减少用高毒性化学物质进行密度分离和在光学显微镜下目视检查颗粒所花费的时间,并且改进的矿物识别和表征可以使地质年代学数据更加可靠。
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
Geochronology
Geochronology Earth and Planetary Sciences-Paleontology
CiteScore
6.60
自引率
0.00%
发文量
35
审稿时长
19 weeks
×
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