Resolución de enigmas geológicos e históricos utilizando técnicas gemológicas avanzadas: Caso del ópalo noble de Franco Dávila (1772)

IF 0.8 4区 地球科学 Q3 GEOLOGY Estudios Geologicos-Madrid Pub Date : 2016-11-24 DOI:10.3989/EGEOL.42459.410
Javier Garcia-Guinea, J. González-Alcalde, M. Furió, A. Jorge, F. Garrido
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Abstract

The large precious opal weighting 33 grams fitted in a silver jewel and exposed to visitors at the Museo Nacional de Ciencias Naturales (MNCN) is well documented in: (i) its own mounting (1772), (ii) at the 775 document of the Archive of the MNCN and (iii) the 395 specimen described in the of Pedro Franco Davila catalogue. The X-ray diffractogram (XRD) performed onto the opal block is very similar to other opals of volcanic origin containing varied amounts of cristobalite, tridymite and amorphous silica. The Raman spectrum shows a band peaked at 242, 343 and 416 cm -1 associated with O-Si-O stretching groups; other spectral band peaked at 780 and 819 cm -1 corresponding to vibration of symmetrical O-Si-O rings of 3 and 4 link members, plus other minor bands. The Raman spectrum is also very similar to those observed in Mexican opals of volcanic origin containing an spectral band of stretching nodes v1 (OH) at 3233, 3393, 3511, 3628 cm -1 related to OH groups with hydrogen bonds of isolated silanol groups. The interferometric confocal dual microscope 3D (MCI3D), which is a nondestructive facility of high resolution and LED technology reveals the geometry of graver tools on the silver jewel and the computed tomography X-ray highlights the opal cutting as a squared princess type and silver chloride infillings of a crack probably caused by a shock on a corner. Under the scanning electron microscope we observed barite, sealed veins of silica rich in Mn and opal with high contents of Al and K which, along with the historical data, the piece can be attributed to the historical site of opals hosted in Slovakia andesite rocks, this data explains the optical light behavior in the cabochon. The silver jewel has large amounts of Hg and AgCl indicating amalgam method. In addition the natural AgS 2 phases probably come from Nueva Espana (year 1772) in full production of silver in such time. The association of new analytical non-destructive techniques combines the preservation of samples together with significant analytical data allowing us to deduce genetic mineral processes, provenances and manufacturing techniques of materials. These facilities allow the characterization, interpretation, conservation and enhancement of cultural and archaeological heritage.
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使用先进的宝石学技术解决地质和历史谜题:以佛朗哥的高贵蛋白石为例davila (1772)
这颗重达33克的大珍贵蛋白石镶嵌在一颗银饰上,在国家自然科学博物馆(MNCN)向游客展示,其详细记录如下:(i)其自身的安装(1772年),(ii)国家自然科学博物馆档案的775年文件,以及(iii)佩德罗·佛朗哥·达维拉目录中描述的395年标本。对该蛋白石块进行的x射线衍射(XRD)与其他火山成因的蛋白石非常相似,含有不同数量的方英石、钇石和无定形二氧化硅。拉曼光谱显示,O-Si-O拉伸基团在242、343和416 cm -1处出现峰值;其他谱带在780和819 cm -1处达到峰值,对应于3和4节元对称O-Si-O环的振动,以及其他较小的谱带。拉曼光谱也与在墨西哥火山源蛋白石中观察到的非常相似,在3233、3393、3511、3628 cm -1处有一个伸展节点v1 (OH)的光谱带,该光谱带与分离的硅烷醇基团的氢键有关。干涉共聚焦双三维显微镜(MCI3D)是一种高分辨率和LED技术的非破坏性设备,揭示了银饰上雕刻工具的几何形状,计算机断层扫描x射线突出显示了蛋白石切割为方形公主型,并且氯化银填充了可能由角上的冲击引起的裂纹。在扫描电镜下观察到重晶石、富锰二氧化硅的封闭脉体和Al、K含量高的蛋白石,结合历史资料,认为该块属于斯洛伐克安山岩中寄存蛋白石的历史遗址,这一数据解释了该块圆块状岩石的光学光行为。银饰有大量的汞和银氯,表明汞齐法。此外,天然的ags2相可能来自新西班牙(1772年),当时白银的全面生产。新的分析非破坏性技术将样品保存与重要的分析数据相结合,使我们能够推断遗传矿物过程,来源和材料的制造技术。这些设施使文化和考古遗产的特征、解释、保护和加强成为可能。
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来源期刊
CiteScore
1.40
自引率
14.30%
发文量
6
审稿时长
>12 weeks
期刊介绍: Since 1945 Estudios Geologicos publishes original research works, as well as reviews, about any topic on Earth Sciences. Estudios Geologicos is published as one yearly volume, divided into two half-yearly issues. It is edited by the Spanish National Research Council (Consejo Superior de Investigaciones Científicas, CSIC) at the Instituto de Geociencias (CSIC-UCM). Estudios Geologicos provides free access to full-text articles through this electronic edition. Accepted articles appear online as "Forthcoming articles" as soon as the galley proofs have been approved by the authors and the Editor-in-Chief. No changes can be made after online publication.
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