首页> 外文期刊>Archaeometry >ARCHAEOMETRIC STUDY OF VOLCANIC LITHIC OBJECTS FROM THE LONGOLA (POGGIOMARINO) PROTOHISTORIC SITE, SOUTHERN ITALY: REGIONAL VERSUS EXTRA-REGIONAL PROVENANCE
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ARCHAEOMETRIC STUDY OF VOLCANIC LITHIC OBJECTS FROM THE LONGOLA (POGGIOMARINO) PROTOHISTORIC SITE, SOUTHERN ITALY: REGIONAL VERSUS EXTRA-REGIONAL PROVENANCE

机译:意大利南部隆戈拉(POGGIOMARINO)原史遗址的火山岩对象的考古学研究:区域对区域外的起源

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The Longola protohistoric village (spanning from the late Middle Bronze Age to the sixth century BC) is a perifluvial settlement located in the Sarno River floodplain to the north-east of Pompeii (southern Italy) and east of the Somma-Vesuvius volcano. A great abundance of artefacts have been found at Longola and in the neighbouring areas, including a variety of volcanic stone objects, mainly related to building and to the manufacture of ordinary tools and instruments. The aim of our work is to characterize lithic objects (lava pebbles and millstones) and to understand their geological provenance by petrographic and geochemical studies. Compositions of millstone samples (porphyritic phonolitic tephrites) and of a set of pebbles (mainly phonolitic tephrites, leucite-shoshonites and trachytes) are compatible with the Somma-Vesuvius magmas erupted before 8 ka BP. For the trachyte lithics, an additional source from the Accademia lava dome (Phlegrean Fields) cannot be ruled out. Among the pebble samples, a rhyolite and a poorly evolved trachyte clearly lie outside the compositional variation of the Somma-Vesuvius and other volcanoes of the Naples area (e.g., Ischia and the Phlegrean Fields) and emphasize an extra-regional provenance. Ponza Island is the best candidate for the provenance of the above two outlier samples.
机译:隆戈拉(Longola)的原始历史村庄(横跨青铜器时代中期至公元前六世纪)是一个河流周边定居点,位于庞贝古城(意大利南部)东北和索马-维苏威火山东部的萨尔诺河河漫滩中。在隆戈拉(Longola)和附近地区,发现了大量的人工制品,包括各种火山石制品,主要涉及建筑和制造普通工具和仪器。我们的工作目的是对岩性物体(熔岩卵石和磨石)进行表征,并通过岩石学和地球化学研究了解其地质来源。磨石样品(斑状的硬质辉绿岩)和一组鹅卵石(主要是硬质性辉绿岩,白云母-长石辉岩和长圆形岩)的成分与8 ka BP之前爆发的索马-维苏威岩浆兼容。对于曲奇石板岩,不能排除来自Accademia熔岩穹顶(Phlegrean Fields)的其他来源。在卵石样品中,流纹岩和发育不良的速溶球显然位于索马-维苏威火山和那不勒斯地区的其他火山(例如伊斯基亚和菲勒格里亚火山场)的成分变化之外,并强调了区域外出处。对于以上两个异常样本的来源,Ponza Island是最佳候选者。

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