mpact Diamonds in an Extravagant Metal Piece Found in Paraguay: Published Raman Spectra revisited

Jaime L.B. Presser, Arif M. Sikder
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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.
在巴拉圭发现的一块奢华金属片中的碎钻:重新审视已发表的拉曼光谱
拉曼光谱分析是对一块 303 千克重的水壶形金属块进行的,该金属块可能含有龙鳞钻石。拉曼光谱显示了四个主要波段:偏移的 D 波段(1294-1330 cm-1)、G 波段(1583-1588 cm-1)、铁陨石波段(217、284 和 402 cm-1)以及微弱的第四波段(1428-1460 cm-1)。全宽均方根值(39-162 cm-1)很高,表明存在大量龙鳞陨石成分(10-100%)。偏移的 D 峰波值和 FWHM 值表明龙闪石金刚石是在高压高温条件下(1068-1541 ℃)形成的,可能是由于太空中的超高速碰撞造成的。这一发现加强了铁陨石中钻石的证据,可能是迄今为止记录到的最大的含钻石铁陨石。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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