Use of ground-probing radar and resistivity surveys for archaeological investigations
Use of ground-probing radar and resistivity surveys for archaeological investigations
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使用地面探测雷达和电阻率测量进行考古调查
DOI：
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发表时间：
1987
期刊：
影响因子：
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通讯作者：
T. Kanemori
中科院分区：
文献类型：
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作者：
T. Imai;T. Sakayama;T. Kanemori
在日本，文物挖掘前通常采用地球物理方法来估计文物的分布。具有考古意义的物体通常位于地表几米之内。因此，适用于考古勘探的地球物理方法是那些在浅层提供高分辨率的方法。最常用的地球物理方法是探地雷达、电阻率和磁力测量。在这些方法中，我们在四个地点的考古调查中主要使用了探地雷达和电阻率测量。其中三个地点位于Gumma县（日本）;这些地点覆盖着火山沉积物（壤土或浮石）。利用地面探测雷达，我们能够定位古民居、土丘和具有考古意义的“文化层”的分布。在另一个地点，在奈良县，我们找到了一个古老城市的部分遗迹。在这项调查中，电阻率法和探地雷达相结合，以确定位置，
In Japan, geophysical methods are normally used to estimate the distribution of cultural relics before digging. Objects of archaeological interest are usually located within a few meters of the surface. Therefore, geophysical methods suitable for archaeological exploration are those which provide high resolution at shallow depths. The most commonly used geophysical methods are ground‐probing radar, resistivity, and magnetometry. Of these methods, we used mainly ground‐probing radar and resistivity surveys in archaeological investigations at four sites. Three of the sites were in Gumma Prefecture (Japan); they were covered with volcanic deposits (loam or pumice). Using ground‐probing radar, we were able to locate ancient dwellings, burial mounds, and a distribution of archaeologically significant “culture layers.” At the other site, in Nara Prefecture, we located part of the remains of an ancient city. In this investigation, the resistivity method and ground‐probing radar were combined to determine the loc...