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Integration of ground-penetrating radar and microgravimetric methods to map shallow caves

机译:探地雷达和微重力方法的集成,用于绘制浅洞

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摘要

Ground-penetrating radar (GPR) and microgravimetric surveys have been conducted in the southern Jura mountains of western Switzerland in order to map subsurface karstic features. The study site, La Grande Rolaz cave, is an extensive system in which many portions have been mapped. By using small station spacing and careful processing for the geophysical data, and by modeling these data with topographic information from within the cave, accurate interpretations have been achieved. The constraints on the interpreted geologic models are better when combining the geophysical methods than when using only one of the methods, despite the general limitations of two-dimensional (2D) profiling. For example, microgravimetry can complement GPR methods for accurately delineating a shallow cave section approximately 10 X 10 mt in size. Conversely, GPR methods can be complementary in determining cavity depths and in verifying the presence of off-line features and numerous areas of small cavities and fractures, which may be difficult to resolve in microgravimetric data. (C) 2001 Elsevier Science B.V. All rights reserved. [References: 24]
机译:为了绘制地下岩溶特征,已在瑞士西部的汝拉山脉南部进行了探地雷达(GPR)和微重力测量。研究地点La Grande Rolaz洞穴是一个广泛的系统,其中绘制了许多部分。通过使用较小的站距和对地球物理数据的仔细处理,以及通过使用来自洞穴内部的地形信息对这些数据进行建模,可以实现准确的解释。尽管二维(2D)轮廓分析存在一般限制,但结合地球物理方法时,对解释的地质模型的约束要比仅使用其中一种方法更好。例如,微重力法可以补充GPR方法,以准确地描绘出大小约为10 X 10 mt的浅洞穴。相反地​​,GPR方法可以在确定型腔深度和验证离线特征以及小空腔和裂缝的大量区域的存在方面是互补的,而这在微重力数据中可能很难解决。 (C)2001 Elsevier Science B.V.保留所有权利。 [参考:24]

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