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ToF-SIMS applied to historical archaeology in the Alps

机译：ToF-SIMS应用于阿尔卑斯山的历史考古

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The actual route Hannibal followed during the invasion of Italia in the Second Punic War is one of the major questions of antiquity, one that historians/archaeologists have long studied. There are six possible passes Hannibal could have used and one of the many bits of evidence in the ancient literature that might help answer this question is the location of fired rock, the result of a conflagration Hannibal is reputed to have employed to reduce the size of boulders in a two-tier blocking rockslide on the lee side (e.g. Italian) some distance down from the high col. The only route with fired rock along the roadway leading to the Po River Valley or the Dora Riparia is below the Col du Clapier, one of the possible northern routes. ToF-SIMS investigation of the 100-mu m thick burned crust in hornblende schist interlaced with veins of quartz-feldspathic minerals yields various elements C, Mg, Na, Ca, Si, Ti, P, Al, Fe and their associated fragments. Hydrocarbon fragments are thought to be products of combustion whereas Ca and Na along with Mg-Fe silicates are derived from the country rock. Aeolian components along with clay minerals settled onto rock surfaces following firing. While the SIMS data clearly would not provide an age for the burnt rock, compositional evidence of the conflagration may relate to Hannibal's actual route. (c) 2006 Elsevier B.V. All rights reserved.
机译：汉尼拔在第二次布匿战争中入侵意大利时所遵循的实际路线是古代的主要问题之一，历史学家/考古学家长期以来一直在研究这一问题。汉尼拔可能使用了六种通行证，而古代文献中许多有助于回答这个问题的证据之一是烧成的岩石的位置，据称汉尼拔发生大火的结果是减小了岩石的尺寸。背风侧（例如，意大利人）的两层阻挡岩石中的巨石，距高high向下一段距离。沿通向波河河谷或多拉里帕里亚（Dora Riparia）的道路的唯一带有烧石的路线是在科尔迪克拉皮尔山脉（Col du Clapier）下，这是可能的北部路线之一。 ToF-SIMS对角闪石片岩中与石英长石矿物脉交错的100微米厚的烧饼进行的调查显示出各种元素C，Mg，Na，Ca，Si，Ti，P，Al，Fe及其相关碎片。碳氢化合物碎片被认为是燃烧产物，而Ca和Na以及Mg-Fe硅酸盐则来自于乡村岩石。烧成后，风沙成分与粘土矿物一起沉积在岩石表面。尽管SIMS数据显然无法提供燃石的年龄，但大火的成分证据可能与汉尼拔的实际路线有关。 （c）2006 Elsevier B.V.保留所有权利。

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