{"title":"mpact Diamonds in an Extravagant Metal Piece Found in Paraguay: Published Raman Spectra revisited","authors":"Jaime L.B. Presser, Arif M. Sikder","doi":"10.32480/rscp.2024.29.1.22","DOIUrl":null,"url":null,"abstract":"Raman spectroscopy analysis was performed on a 303 kg pitcher-shaped metal piece, likely bearing lonsdaleite diamonds. The Raman spectra revealed four main bands: a shifted D-band (1294-1330 cm-1), a G-band (1583-1588 cm-1), an iron meteorite band (217, 284, and 402 cm-1), and a weak fourth band (1428-1460 cm-1). FWHM values (39-162 cm-1) were high, indicative of a significant lonsdaleite component (10-100%). The shifted D-peak wavenumber and FWHM values suggest the formation of lonsdaleite diamonds under high-pressure, high-temperature conditions (1068-1541 °C), possibly due to a hypervelocity collision in space. This finding strengthens the evidence for diamonds in iron meteorites and could represent the largest diamond-bearing iron meteorite recorded to date.","PeriodicalId":516094,"journal":{"name":"Revista de la Sociedad Científica del Paraguay","volume":"38 5","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Revista de la Sociedad Científica del Paraguay","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.32480/rscp.2024.29.1.22","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Raman spectroscopy analysis was performed on a 303 kg pitcher-shaped metal piece, likely bearing lonsdaleite diamonds. The Raman spectra revealed four main bands: a shifted D-band (1294-1330 cm-1), a G-band (1583-1588 cm-1), an iron meteorite band (217, 284, and 402 cm-1), and a weak fourth band (1428-1460 cm-1). FWHM values (39-162 cm-1) were high, indicative of a significant lonsdaleite component (10-100%). The shifted D-peak wavenumber and FWHM values suggest the formation of lonsdaleite diamonds under high-pressure, high-temperature conditions (1068-1541 °C), possibly due to a hypervelocity collision in space. This finding strengthens the evidence for diamonds in iron meteorites and could represent the largest diamond-bearing iron meteorite recorded to date.