首页> 外文期刊>Journal of Archaeological Science >Ground-penetrating radar investigations at Marj Rabba, a Chalcolithic site in the lower Galilee of Israel
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Ground-penetrating radar investigations at Marj Rabba, a Chalcolithic site in the lower Galilee of Israel

机译:在以色列下加利利的黄铜矿遗址Marj Rabba进行的探地雷达调查

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摘要

The Chalcolithic site of Marj Rabba, in the lower Galilee of Israel, features shallow limestone structures situated in a terra rossa matrix. Calcareous substrates such as terra rossa, common throughout the region, are often not considered amenable to ground-penetrating radar (GPR) studies due to strong attenuation, particularly within the relatively high frequency range most often used in archaeological GPR surveys. Energy loss due to scattering from small embedded stones also exacerbates attenuation at this particular site in addition to obscuring detected archaeological features, thereby complicating interpretation. Because features are fairly shallow (upper 1.5 m) and contrast well with the soil, however, GPR was successful in spite of poor substrate quality. The selection of a somewhat lower antenna frequency (250 MHz) than is often recommended for archaeology, played a role in the success of the work. The end result expands the known spatial extent of the site by five-fold, increasing our knowledge of architectural and village plans for a time period which is poorly understood in this region. The settlement scale and complexity shown by these new results indicates that Chalcolithic villages are not only present in the Galilee but are as extensive and architecturally sophisticated as contemporaneous settlements in other regions. In combination with excavation results, the structures detected with GPR at Marj Rabba provide the largest plan of an early Chalcolithic settlement in the Galilee.
机译:位于以色列下加利利的玛尔·拉巴(Maj Rabba)的石器时代遗址,其浅色石灰岩结构位于terra rossa矩阵中。在整个区域中常见的钙质基质(例如terra rossa),由于强烈衰减,特别是在考古GPR勘测中最常使用的相对较高的频率范围内,通常不被认为适合地面穿透雷达(GPR)研究。除了掩盖检测到的考古特征外,由于从小嵌入石块散射而导致的能量损失还加剧了该特定位置的衰减,从而使解释变得复杂。因为特征很浅(1.5 m以上)并且与土壤形成了很好的对比,所以尽管基底质量较差,GPR还是成功的。选择比考古学通常推荐的更低的天线频率(250 MHz),对工作的成功起到了作用。最终结果将场地的已知空间范围扩大了五倍,从而增加了我们对该地区建筑和乡村规划的了解,这一时期对此地区了解甚少。这些新结果表明的定居规模和复杂性表明,加利利的不仅有石器时代的村庄,而且与其他地区的同时定居点一样,其范围和结构也很复杂。结合开挖结果,在Marj Rabba用GPR探测到的结构为加利利的早期石器时代聚落提供了最大的计划。

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