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.