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This project follows on from an initial study of Celtic gold coins from the Middle Rhine/Moselle region, which was based on material found at the Martberg, a Late Iron Age/Roman sanctuary and settlement (River Moselle, western Germany; Bendall 2003 ). The earlier work was expanded to encompass over 100 examples of various other regional Celtic gold coinages from the collection of the Römisch‐Germanisches Zentralmuseum, Mainz. The alloy (Au–Ag–Cu) and trace element compositions (in particular Ni, Sb and Pt) were determined by EPMA and LA–ICP–MS, respectively, and their Pb isotope signatures were measured by LA–MC–ICP–MS. Of the 28 trace elements measured, only Ni, Sb and Pt were found to show meaningful variations and so only they are presented here. In particular, differences in the Pt/Au ratios between various groups of earlier coinage (imitations of Philippus and Alexander/Nike staters, Sch. 23 and some early Boian coins) on the one hand, and the majority of the Boian and the southern rainbow cup coinages on the other, indicate a significant difference in the gold sources exploited for these regional coinages. The Pb isotope data confirm previous conclusions that the contribution of gold to the total lead in the Au–Ag–Cu coin alloys can be detected, especially for coins with over 70% gold, and show that possible gold sources include both eastern Mediterranean and Alpine sources. Combining the Pb isotope data with the Pt/Au ratios allows the potential gold sources to be further differentiated.  相似文献   
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Iron finds from the Celtic oppidum of Manching in southern Bavaria (Germany) are analysed in view of their possible provenance. The exceptional size and the location of Manching are usually attributed to the presence of abundant iron ores in its vicinity. After a review of previous approaches for source determination of iron artefacts, we introduce lead isotope analysis as a new approach. However, only by combining the trace element patterns of slag inclusions and iron metal with lead isotope ratios in the metal is it possible to distinguish various iron ore formations near Manching. As a result, it turns out that, indeed, the most obvious ones—namely, bog ores near the Danube—constituted the main resources for iron production at Manching. It was even possible to select one occurrence as the most likely ore source.  相似文献   
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《Public Archaeology》2013,12(2):85-107
Abstract

'Welcome to Tintagel, the birthplace of King Arthur' is a phrase often repeated at this small village on the north coast of Cornwall where legend, childhood stories and merchandise all serve to attract thousands of visitors per year. As 'a place to go', the area provides stunning coastal scenery, a romantic ruined castle and a highly commercialised village. Tintagel Island, owned by the Duchy of Cornwall but managed by English Heritage, plays centre stage as the 'birthplace' in question. On-site, the character of Arthur is largely debunked as a literary phenomenon and, furthermore, a survey of day-trippers revealed that visitors were left in an interpretive limbo — arriving with ideas of Arthur and leaving knowing little about Tintagel.

Whilst the aesthetics of the castle and scenery go some way towards mitigating against disappointment, on site encounters with kitsch representations of the past combine with more amorphous senses of pseudo-spiritual atmospheres as well as experiences of walking, eating and drinking to ultimately provide a 'grand day out'. The marketing ephemera and heritage presentation all serve to create, reinforce and suppress different identities of place which are revealed as being a fairly cohesive package of Celtic-Arthuriana. This paper questions the ways in which visitors' expectation and imagination are mediated through experience of place.  相似文献   
4.
N. BRUN  M. PERNOT 《Archaeometry》1992,34(2):235-252
Opaque red glass was used in the Celtic world for enamels and inlays. Forty artefacts, of various dates and found in various places, have been sampled and studied. They all belong to the same type, a soda-lime-silica high lead glass coloured by crystals of cuprous oxide. There is only one subgroup: glass lumps from the Mont-Beuvray oppidum contain manganese, less iron, and less lead. This change could be the result of Roman influence. Although most of these glasses form a surprisingly homogeneous group, no conclusions as to their origin can be inferred from our present knowledge.  相似文献   
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