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Platinum group placer minerals in ancient gold artifacts - Geochemistry and osmium isotopes of inclusions in Early Bronze Age gold from Ur/Mesopotamia

机译:古代金器中的铂族砂金矿物-Ur /美索不达米亚早期青铜时代金矿中夹杂物的地球化学和同位素

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One of the most significant characteristics of the gold artifacts from the Early Dynastic Royal Tombs of Ur, Mesopotamia are numerous inclusions consisting of the platinum group elements (PGE) osmium iridium ruthenium. In nature, minerals of PGE (PGM) are enriched along with gold and other heavy minerals in placer deposits. During metallurgical gold extraction from placer material and subsequent production of artifacts, PGMs were incorporated in the gold artifacts due to their refractoriness almost unmodified. In order to evaluate their potential for provenance studies of gold, the PGE inclusions were analyzed for their chemical and Os-isotope compositions. They contain highly variable concentrations of Os (26-70 wt.%), Ir (14-62 wt.%) and Ru (0.4-45 wt.%). Os-187/Os-188 isotope ratios vary between 0.118 und 0.178. Due to the high Ru content of the alloys, the chemical composition point to a geological context of ophiolite complexes. Os isotope ratios are a powerful tool to narrow down the potential ore sources for the gold. However, the interpretation of calculated model ages is difficult due to the unknown genesis of the parental magma. Calculated ages (290-610 Ma) for measured Os-187/Os-188 of 0.125 using different reference values could indicate placers close to Paleozoic ophiolites like Samti (Takhar) in Northern Afghanistan and Zarshouran (Western Azerbaijan) in Iran, but need to be confirmed by additional measurements of their Os isotope signature in the future. Other archaeological relevant sources of PGM and gold could be excluded by direct comparison of their Os isotope data: 1.) old Neoproterozoic ophiolites from the Eastern Desert type (750-800 Ma), Egypt, 2.) young Mesozoic ophiolites from the Samail complex (96 Ma) in Oman. Thus, in combination with other tracers the Os isotope ratio is a valuable source for provenance studies. (C) 2016 Elsevier Ltd. All rights reserved.
机译:美索不达米亚Ur朝代王朝早期皇家陵墓中的金器物最显着的特征之一就是包含铂族元素(PGE)铱钌的许多包裹体。在自然界中,PGE(PGM)矿物与金和其他重矿物一起在砂矿中富集。在从砂矿材料中提取冶金金并随后生产伪影的过程中,由于铂金的耐火度几乎未改变,因此将PGM掺入了黄金伪影中。为了评估其在金的来源研究中的潜力,对PGE夹杂物的化学和Os同位素组成进行了分析。它们包含浓度高度可变的Os(26-70 wt。%),Ir(14-62 wt。%)和Ru(0.4-45 wt。%)。 Os-187 / Os-188同位素比在0.118和0.178之间变化。由于合金中Ru含量高,化学成分指向蛇绿岩配合物的地质环境。 s同位素比是缩小金的潜在矿石来源的有力工具。但是,由于父母岩浆的成因未知,因此很难解释计算出的模型年龄。使用不同的参考值得出的Os-187 / Os-188测得的年龄(290-610 Ma)为0.125(使用不同的参考值)可能表明砂岩接近古生蛇绿岩,如阿富汗北部的Samti(Takhar)和伊朗的Zarshouran(西阿塞拜疆),将来可通过对其Os同位素特征的其他测量来确认。通过直接比较它们的Os同位素数据,可以排除PGM和金的其他与考古有关的来源:1.)来自埃及东部沙漠型(750-800 Ma)的旧新元古代蛇绿岩; 2.)来自Samail复杂群的年轻中生蛇绿岩(96 Ma)在阿曼。因此,与其他示踪剂结合使用时,Os同位素比率是出处研究的重要来源。 (C)2016 Elsevier Ltd.保留所有权利。

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