Combined external-beam PIXE and μ-Raman characterisation of garnets used in Merovingian jewelry

被引:59
作者
Calligaro, T
Colinart, S
Poirot, JP
Sudres, C
机构
[1] CNRS, Ctr Rech & Restaurat Musees France, UMR 171, F-75041 Paris 01, France
[2] Univ Paris 01, F-75006 Paris, France
关键词
PIXE; garnet; jewel; provenance; Merovigians;
D O I
10.1016/S0168-583X(01)01078-3
中图分类号
TH7 [仪器、仪表];
学科分类号
0804 ; 080401 ; 081102 ;
摘要
Red garnets were the dominant gemstones used for jewels in Europe during the Early Middle Ages, We have studied over 350 garnets set on 12 jewels unearthed in the royal necropolis of the Saint-Denis Basilica, close to Paris, This famous collection of "cloisonne" style artefacts dates from the Merovingian period (late fifth century AD to early seventh century AD). The archaeological issue addressed is the identification of the geographical origin of these garnets, in view to establish the gem trading routes during the Dark Ages. External beam PIXE was used to determine the major constituents (Mg. Al. Si, Ca, Mn. Fe), specifying the garnet type (composition in various mineralogical end-members, e.g. almandine. pyrope. spessartite,...) and the trace element content (Cr, Y). Three sorts of garnets were identified. Ten jewels are adorned with almandine garnets (Fe-rich). One jewel has intermediate almandine-pyrope garnets ("rhodolite"). The last and most recent jewel is inlaid with pyrope (Mg-rich,) garnets. Trace element content and slight differences in major composition allowed to distinguish five different sources: two sources for pyrope garnets (with and without chromium), and two sources for almandine garnets (distinctive calcium, magnesium and yttrium contents). A preliminary comparison with literature data suggested that almandine garnets may have been mined from India while the "rhodolite" garnets may have been imported from Sri Lanka. The sources of pyrope garnets could be the Bohemian deposits (Czech republic). In addition. mu-Raman spectrometry was used to identify most of the mineral inclusions (apatite. zircon, ilmenite, monazite, calcite, quartz) present in almandine garnets, Even if two specific types of inclusions were not identified. due to the lack of corresponding reference spectra in our database, the Raman spectra collected provided an interesting inclusion fingerprint. (C) 2002 Elsevier Science B,V, All rights reserved.
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页码:320 / 327
页数:8
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