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一种鉴定古代白色大理石来源的创新方法:X射线衍射在厘清戈克泰佩大理石和卡拉拉大理石来源方面的贡献。

An innovative approach for provenancing ancient white marbles: the contribution of x-ray diffraction to disentangling the origins of Göktepe and Carrara marbles.

作者信息

Antonelli F, Nestola F

机构信息

LAMA - Laboratory for Analysing Materials of Ancient Origin, IUAV University of Venice, San Polo, 2468, 30125, Venezia, Italy.

Department of Geosciences, University of Padova, Via G. Gradenigo 6, 35131, Padua, Italy.

出版信息

Sci Rep. 2021 Nov 16;11(1):22312. doi: 10.1038/s41598-021-01800-7.

DOI:10.1038/s41598-021-01800-7
PMID:34785752
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8595683/
Abstract

The paper presents a very efficient, quick, low-cost and minimally micro-destructive approach to discriminating between Roman artefacts sculpted with Göktepe (Aphrodisia, Turkey) or Carrara (Apuan Alps, Italy) white marbles by using a standard X-Ray Powder Diffractometer (XRPD) and a refinement of the unit cell parameters and volume of calcite. At present, the routine way of differentiating between these two almost indistinguishable by-eye marbles is based on the typically higher strontium content of calcite in the Microasiatic lithotype, a unique geochemical-crystallographic feature with respect to all other non-Göktepe fine-grained white marbles used in classical times. The XRPD approach has been verified by testing eighteen samples of known composition, nine from Carrara and nine from Göktepe quarries, which had already been analysed with other laboratory techniques. The applicability of the method to archaeological artefacts was confirmed by an archaeometric study performed on some famous Roman sculptures of the National Archaeological Museum of Venice and from Hadrian's Villa at Tivoli. The results show that Göktepe/Carrara discrimination is always possible and that this XRPD approach can potentially become a useful and low-cost routine procedure to solve provenance issues.

摘要

本文提出了一种非常高效、快速、低成本且微破坏性极小的方法,通过使用标准的X射线粉末衍射仪(XRPD)以及对方解石晶胞参数和体积的细化,来区分用土耳其阿弗罗狄西亚的戈克泰佩白大理石或意大利阿普安阿尔卑斯山的卡拉拉白大理石雕刻的罗马文物。目前,区分这两种肉眼几乎无法区分的大理石的常规方法是基于小亚细亚岩性中方解石通常较高的锶含量,这是一种相对于古典时期使用的所有其他非戈克泰佩细粒白色大理石而言独特的地球化学-晶体学特征。XRPD方法已通过对18个已知成分的样品进行测试得到验证,其中9个来自卡拉拉,9个来自戈克泰佩采石场,这些样品已经用其他实验室技术进行了分析。通过对威尼斯国家考古博物馆和蒂沃利哈德良别墅的一些著名罗马雕塑进行的考古计量学研究,证实了该方法对考古文物的适用性。结果表明,区分戈克泰佩/卡拉拉大理石总是可行的,并且这种XRPD方法有可能成为解决产地问题的一种有用且低成本的常规程序。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0f1c/8595683/8b6ac744ee25/41598_2021_1800_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0f1c/8595683/3e7766971a82/41598_2021_1800_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0f1c/8595683/3445a48634cd/41598_2021_1800_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0f1c/8595683/f2dd02bf8ae0/41598_2021_1800_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0f1c/8595683/6d7e830a281c/41598_2021_1800_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0f1c/8595683/8a6c1155869c/41598_2021_1800_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0f1c/8595683/8b6ac744ee25/41598_2021_1800_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0f1c/8595683/3e7766971a82/41598_2021_1800_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0f1c/8595683/3445a48634cd/41598_2021_1800_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0f1c/8595683/f2dd02bf8ae0/41598_2021_1800_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0f1c/8595683/6d7e830a281c/41598_2021_1800_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0f1c/8595683/8a6c1155869c/41598_2021_1800_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0f1c/8595683/8b6ac744ee25/41598_2021_1800_Fig6_HTML.jpg

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本文引用的文献

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Fundamental Parameters Line Profile Fitting in Laboratory Diffractometers.实验室衍射仪中的基本参数线轮廓拟合
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