Going Inside a Historical Brazilian Diamond from the Spada Collection (19th Century)

IF 2.4 4区 材料科学 Q2 CRYSTALLOGRAPHY Crystals Pub Date : 2024-08-31 DOI:10.3390/cryst14090779
Giovanna Agrosì, Daniela Mele, Gioacchino Tempesta
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Abstract

The characterization of objects of historical and cultural interest represents a crucial topic, specifically when it regards gemstones. Actually, the advanced investigation of precious minerals of gemological interest requires exclusively non-destructive analyses which are also suitable for determining their provenance when it is unknown. In this study, a non-destructive analytical protocol, previously tested on diamonds for petrogenetic studies, has been applied to a natural diamond of very high historical and gemological value, donated in 1852 by Monsignor Lavinio de ‘Medici Spada to the Museum of Earth Sciences of Sapienza University (Rome). The analytical protocol used includes X-ray diffraction topography, micro-computed X-ray tomography, single-crystal micro-X-ray diffraction and Fourier-transform infrared spectroscopy. The results show the presence of dislocations originating from inclusions and a very low degree of plastic deformation. The aggregation states of its N impurities show that this diamond is type IaAB, while the inclusions consist of olivine (Fo92-93), suggesting a lithospheric origin. The historical references found in the catalogs of the Museum indicate only a Brazilian origin, without any reference to the mining district. The information acquired in this study, enhanced by document research on mining in Brazil since 1700, suggests that the diamond likely comes from the district of Diamantina, Mina Gerais, Brazil.
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走进斯帕达收藏的一颗历史悠久的巴西钻石(19 世纪)
具有历史和文化价值的物品的特征描述是一个至关重要的课题,特别是在宝石方面。事实上,要对具有宝石学价值的珍贵矿物进行深入研究,就必须进行专门的非破坏性分析,这种分析也适用于在来源不明的情况下确定其出处。在这项研究中,先前在钻石上测试过的用于岩石学研究的非破坏性分析方案,已被应用于一颗具有极高历史和宝石学价值的天然钻石,这颗钻石是由 Monsignor Lavinio de 'Medici Spada 于 1852 年捐赠给罗马萨皮恩扎大学地球科学博物馆的。所使用的分析方案包括 X 射线衍射拓扑图、微观 X 射线层析成像、单晶微 X 射线衍射和傅立叶变换红外光谱。结果表明,存在源自夹杂物的位错,塑性变形程度很低。其 N 杂质的聚集状态表明这块钻石属于 IaAB 型,而包裹体由橄榄石(Fo92-93)组成,表明其来源于岩石圈。博物馆目录中的历史参考资料仅表明其产地为巴西,但未提及矿区。通过对 1700 年以来巴西采矿情况的文献研究,本研究获得的信息表明,这颗钻石很可能来自巴西米纳吉拉斯的 Diamantina 地区。
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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来源期刊
Crystals
Crystals CRYSTALLOGRAPHYMATERIALS SCIENCE, MULTIDIS-MATERIALS SCIENCE, MULTIDISCIPLINARY
CiteScore
4.20
自引率
11.10%
发文量
1527
审稿时长
16.12 days
期刊介绍: Crystals (ISSN 2073-4352) is an open access journal that covers all aspects of crystalline material research. Crystals can act as a reference, and as a publication resource, to the community. It publishes reviews, regular research articles, and short communications. Our aim is to encourage scientists to publish their experimental and theoretical results in as much detail as possible. Therefore, there is no restriction on article length. Full experimental details must be provided to enable the results to be reproduced. Crystals provides a  forum for the advancement of our understanding of the nucleation, growth, processing, and characterization of crystalline materials. Their mechanical, chemical, electronic, magnetic, and optical properties, and their diverse applications, are all considered to be of importance.
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