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Karstic morphologies identified with geophysics around saulges caves (Mayenne, France)

机译:通过Saulges洞穴周围的地球物理学识别的岩溶形态(法国马耶讷)

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摘要

Geophysical measurements were carried out around Saulges caves that sought to highlight the local karstic morphologies and the impact on preservation of archaeological material withi n the caves. Electrical resistivity tomographies (ERTs) and apparent conductivity mapping detected a soil cover on the plateaus that ends abruptly over fractured limestone or over a bowl-shaped structure filled with clay soil. Moreover, there is at least one zone of soil accumulation with a basin form with almost no soil cover around this structure. The ERTand seismic refraction tomography (SRT) detected an important anomaly in the valley. Many clues indicate that this anomaly is a karstic conduit filled with water orclay.Therefore, some karstic dissolution zones have been found and only geophysical methods are able to detect such features. Detection of preferential pathways could help to protect prehistoric art within the caves and new karstic morphologies help to better understand this karstic system.
机译:在索尔格斯(Sauges)洞穴周围进行了地球物理测量,旨在突显当地的岩溶形态以及对洞穴的考古材料保存的影响。电阻层析成像(ERTs)和表观电导率图谱检测到高原上的土壤覆盖层,该覆盖层在破裂的石灰岩或充满粘土的碗形结构上突然终止。此外,至少有一个土壤堆积区,呈盆状,周围几乎没有土壤覆盖。 ERT和地震折射层析成像(SRT)在山谷中发现了一个重要异常。许多线索表明该异常是充满水或粘土的岩溶导管,因此,已发现一些岩溶溶解带,只有地球物理方法才能探测到这种特征。检测优先通道可以帮助保护洞穴内的史前艺术,新的岩溶形态有助于更好地了解该岩溶系统。

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