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Variability in pottery production at Khalet al-Jam'a necropolis, Bethlehem (West Bank): From the Early-Middle Bronze to the Iron Age

机译:伯雷特·贾马·墓地,伯利恒(西岸)陶器生产的可变性:从早期的青铜到铁时代

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Rescue excavations undertaken by Sapienza University of Rome and the Palestinian Ministry of Tourism and Antiquities, Department of Archaeology and Cultural Heritage (MOTA-DACH) revealed a huge necropolis in the site of Khalet al-Jam'a, south-east of Bethlehem. Tombs were used during the Early Bronze IV (2300-2000 BCE) to Middle Bronze I-III (2000-1500 BCE) periods, and up to the Iron Age IB-II (1050-700 BCE). This paper presents the results of the minero-petrographic and chemical characterization of ceramic material from this site, with the aim to reconstruct the technological level achieved by ancient populations living in Bethlehem from the Early Bronze IV to the Iron Age by means of optical microscopy, X-ray Powder Diffraction, Scanning Electron Microscopy with Energy Dispersive Spectroscopy and Thermogravimetric Analysis. Results show that two main supplies of raw materials can be recognized at Khalet al-Jam'a. The Early and Middle Bronze Age ceramic production is made with the so-called Moza-clay: a calcareous-rich clay with predominant limestone, diffuse grains of calcite, dolomite, and rare sedimentary siliceous rock fragments, quartz and microfossils. The latest production, namely that of the Iron Age, is more likely consistent with the calcareous-foraminiferous-Rendzina soil clay, with predominant silty quartz and few microfossils. The firing temperature was estimated from the mineralogical assemblage in each sample. Abundant calcite, clay minerals and the absence of neo-formed minerals suggest samples fired at temperatures lower than 800 degrees C. For those samples where calcite was found along with gehlenite and wollastonite, the temperature was indeed estimated to be in the range 850-950 degrees C. Finally, the firing atmosphere was uncontrolled, as testified by the extreme variability in colour of the matrix. The results of this study enable a preliminary characterization of pottery, whose production shows differences related to specific historical periods and contribute to improve the knowledge about specific ceramic production used in funerary contexts.
机译:Sapienza罗马大学和巴勒斯坦旅游和古地,考古和文化遗产部(Mota-Dach)开展的救援挖掘(Mota-Dach)在伯利恒东南部的Khalet Al-jam'a网站上揭示了巨大的墓地。在早期青铜IV(2300-2000 BCE)期间使用墓葬到中间青铜I-III(2000-1500 BCE)期间,达到铁代时IB-II(1050-700 BCE)。本文介绍了来自该地点的陶瓷材料的米洛岩石和化学表征的结果,目的是通过光学显微镜从早期青铜IV到伯利恒生活在伯利恒的古代人群实现的技术水平, X射线粉末衍射,扫描电子显微镜与能量分散光谱和热重分析。结果表明,在哈利埃尔·贾马的哈利特·贾马省可以识别出原料的两个主要用品。早期和中古青铜时期陶瓷生产由所谓的Moza-Clay制成:一种富含钙质的石灰石的钙质粘土,方解石,白云石和稀有沉积硅质岩石片段,石英和微碎石的漫反射颗粒。最新的生产,即铸铁时代,更有可能与钙质传染率 - 林义泥粘土一致,具有主要的粉质石英和少量微生物。从每个样品中的矿物组合估计烧制温度。丰富的方解石,粘土矿物质和没有新成型矿物质的缺失表明样品在低于800℃的温度下烧制的样品。对于那些先驱和硅灰石和硅灰石发现方解石的样品,该温度确实估计在850-950范围内最终,烧制气氛是不受控制的,如通过基质颜色的极端变异而作证。该研究的结果能够初步表征陶器,其生产表现出与特定历史时期相关的差异,并有助于改善对丧葬环境中使用的特定陶瓷生产的知识。

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