Sumaki Höyük (Batman, Türkiye) Neolitik Yerleşiminde Bulunan Bazalt Parçalarının Çok Perspektifli Jeokimyasal ve Mineralojik Analizi

IF 0.4 Q4 GEOSCIENCES, MULTIDISCIPLINARY Turkiye Jeoloji Bulteni-Geological Bulletin of Turkey Pub Date : 2023-07-29 DOI:10.25288/tjb.1310550
Savaş Sarialtun, Mustafa Avcioğlu, Mahmut Aydin
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Abstract

This study aims to determine the provenance of grinding stone tools unearthed from the Neolithic phases of Sumaki Höyük settlement using a portable Energy Dispersive X-ray Fluorescence Spectrometer (P-EDXRF) and X-ray Diffraction spectrometer (XRD). Sumaki Höyük is located in the Lower Garzan Basin of Batman province, Turkey. The settlement is dated to 9084 - 8123 cal BP. Grinding stone tools in this settlement are usually made of basalt. Albeit at low amounts, limestone was also used in the production of grinding stones. The Lower Garzan Basin, located to the east of Diyarbakır Basin, is surrounded by Mount Kıradağı and Mount Raman to the west and the Garzan and Kentalan Anticlinal to the east with Kıradağı extending in a northwest-southeast direction. The basalt flow occurred in the Quaternary period. Samples collected from different parts of the Neolithic phase of Sumaki Höyük and the Kıradağı basalt flows were analyzed using P-EDXRF to determine their chemical composition. The same samples were also analyzed using XRD to determine their mineral composition. P-EDXRF and XRD analyses reveal that the samples from Sumaki Höyük and Kıradağı are in good accordance with each other. It is therefore understood that the basalt stone tools used in the settlement were taken from the Kıradağı basalts. Data gathered on the characteristics of potential source locations provide an insight into the settlement strategy and mobility of Neolithic communities.
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Sumaki Höyük
本研究旨在利用便携式能量色散x射线荧光光谱仪(P-EDXRF)和x射线衍射光谱仪(XRD)确定Sumaki Höyük聚落新石器时期出土的磨石工具的来源。Sumaki Höyük位于土耳其巴特曼省的下加尔赞盆地。该定居点可追溯到9084 - 8123 cal BP。这个聚落的磨石工具通常是由玄武岩制成的。尽管数量很少,石灰石也被用于生产磨石。下加尔赞盆地位于Diyarbakır盆地的东部,西部为Kıradağı山和拉曼山,东部为加尔赞和肯塔兰背斜,Kıradağı向西北-东南方向延伸。玄武岩流发生于第四纪。利用P-EDXRF分析了Sumaki Höyük新石器时代不同部位和Kıradağı玄武岩流的样品,以确定其化学成分。同样的样品也用XRD进行了分析,以确定其矿物组成。P-EDXRF和XRD分析表明,Sumaki Höyük和Kıradağı样品的一致性很好。因此可以理解,在定居点中使用的玄武岩石器是从Kıradağı玄武岩中提取的。收集到的关于潜在来源位置特征的数据提供了对新石器时代社区的定居策略和流动性的深入了解。
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