The metallurgy of the bronze age artifacts from the Shaitanska site (north of Ekaterinburg) of the Sejmo-Turbino type in Eurasia

在欧亚大陆，在芬兰和阿尔泰山脉之间的森林地带，从公元前2000年左右到公元2000年的前半段，在广阔的地理区域内发现了Sejma-Turbino类型的人工制品，它们在类型学上是相同的。他们像<s:1>套轴一样有着令人惊讶的高级类型学发展。自2004年以来，乌拉尔山脉以东的沙杰坦斯卡湖（Ozero II）上的一个新遗址开始为人所知，在那里，从塞伊马-图比诺型中挖掘出了130多件金属文物。我们在跨乌拉尔山脉的辛塔什塔文化强化定居点地区的研究首次展示了对人工制品和矿石的地球化学分析。在此应用程序中，将对50个选定的人工制品和10个矿石样品进行地球化学分析。它的目标是从塞伊玛-图比诺文物中获得第一批大型系列数据。这些数据将作为与南乌拉尔山脉进行比较的基础，并与来自波鸿的Thomas Stöllner领导的研究小组合作，将新数据与来自哈萨克斯坦的许多矿石和人工制品分析一起进行评估和比较。在乌拉尔和阿尔泰之间的大空间内，获得矿床的同位素特征、分布和金属分布网络的初步基础资料和信息是一个重要的目标。第二个目标是锡合金与砷合金的关系的开始问题。最后，根据铅同位素数据，研究Sejma-Turbino型人工制品的起始材料在多大程度上可以归因于不同的区域矿石来源，以及是否可以获得关于该人工制品群传播机制的陈述。

In Eurasia are found in the forest zone between Finland and the Altai mountains over a wide geographical area from around 2000 BC and in the first half of the 2nd millennium artifacts of the type Sejma-Turbino, which are typologically the same. They have like the Tüllenbeile (soket axes) a surprisingly advanced typological development. Since 2004, east of the Urals, a new site on the Shajtanska Lake (Ozero II) is getting known, where more than 130 metal artifacts were excavated from the type Sejma-Turbino. Our research in the Trans-Urals in the area of the fortified settlements of the Sintashta culture have shown first geochemical analyzes of artifacts and ores. In this application 50 selected artifacts and 10 ore samples shall be analyzed geochemically. It is the aim to get a first large series of data from Sejma-Turbino artefacts. The data shall be the basis for comparison with the southern Trans-Urals and in collaboration with the research group led by Thomas Stöllner from Bochum, the new data should be evaluated and compared together with the many ore and artifact analysis from Kazakhstan. It is an important goal to get first basic data and information on the isotopic character of the ore deposits, on the distribution and on the networks of the metal distribution in these large spaces between Ural and Altai. A second objective is the question of the beginning of tin alloys in relation to arsenic alloys. Last to be studied based on the lead isotope data, is the extent to which the starting material of the artifacts of the type Sejma-Turbino can be attributed to different regional ore sources and if statements can be obtained on the mechanism of spread of this artifact group.