...
首页> 外文期刊>Journal of Archaeological Science >A lead-isotope database of copper ores from the Southeastern Alps: A tool for the investigation of prehistoric copper metallurgy
【24h】

A lead-isotope database of copper ores from the Southeastern Alps: A tool for the investigation of prehistoric copper metallurgy

机译:东南阿尔卑斯山脉铜矿石的铅同位素数据库:史前铜冶金研究的工具

获取原文
获取原文并翻译 | 示例
           

摘要

The Southeastern Alps were an important source of copper metal in prehistory, at least from the Eneolithic and through the Bronze Age, as documented by the abundant and substantial presence of smelting slags. Evidence of mining activity is scarce, because of limited ad hoc investigation and because of the subsequent systematic erasing by post-Medieval exploitation. Moreover, until recently the profusion of archaeometallurgical and archaeological investigations focusing on the prehistoric exploitation of Northern Alpine, Central European, and Balkan ore sources has somehow obscured the early role of the Italian Southern Alps as a major copper producing area. The recent advances in the systematic characterization of the copper ores in the Southeastern Alps (including Alto Adige, Trentino, Veneto, and nearby regions) by lead isotope analysis, supported by mineralogical and geochemical interpretation, offer now the appropriate tools to re-evaluate the extent of prehistoric mining and the local patterns of ore exploitation. The developed database is a powerful tool to identify the metal derived from local production. It is suggested that (1) based on the abundance and chronological distribution of smelting slags evidence, two major periods of mining exploitation took place, the first in the middle of the 3rd millennium BC and the second during the Late Bronze Age; and (2) based on the discrimination of copper sources and the available analyses, most of the metal circulating in Northern Italy and in the greater Po Valley region was actually produced from Southern Alpine ores. (C) 2016 Elsevier Ltd. All rights reserved.
机译:东南阿尔卑斯山是史前时期铜金属的重要来源,至少从Eneolithic到整个青铜时代都有,熔渣的大量存在证明了这一点。由于有限的临时调查以及随后的中世纪后剥削活动,采矿活动的证据很少。此外,直到最近,大量的考古学和考古学研究都集中在史前对北部高山,中欧和巴尔干矿石的开采,这在某种程度上掩盖了意大利南部阿尔卑斯山作为主要铜矿产区的早期作用。在矿物学和地球化学解释的支持下,通过铅同位素分析对东南阿尔卑斯山(包括奥拓阿迪杰,特伦蒂诺,威尼托和附近地区)的铜矿石进行系统表征的最新进展,现在提供了适当的工具来重新评估铜矿。史前采矿的范围和当地的矿产开采方式。开发的数据库是识别本地生产的金属的有力工具。建议(1)根据熔渣证据的丰富性和时间分布,发生了两个主要的采矿开采时期,第一个时期是在公元前3世纪中期,第二个时期是在青铜时代。 (2)根据对铜源的区分和现有的分析,在意大利北部和大波河谷地区循环的大多数金属实际上是从南部高山矿石中生产的。 (C)2016 Elsevier Ltd.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号