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High-resolution ground penetrating radar imaging (225- to 900-MHz) of geomorphic and geologic settings: examples from Utah Washington and Wisconsin

机译:高分辨率地面穿透雷达成像(225至900-MHz)的地貌和地质环境:来自犹他州华盛顿和威斯康星州的例子

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Over the past 10 years, ground penetrating radar (GPR) studies in a wide variety of geomorphic and geologic settings have, surprisingly, revealed detailed stratigraphic information. Most of these studies were conducted with lower frequency antennae (50 - 100 MHz) in an effort to better understand subsurface stratigraphy. As GPR systems and data collection methods continue to improve in their ability to collect higher quality digital data, GPR investigations are poised to enter a new era of higher resolution exploration utilizing higher frequency antennae. The paper presents the results of four case studies using a higher frequency (225 - 900 MHz) GPR system to effectively investigate coastal and eolian sedimentary environments. Some drawbacks of higher frequency data are: the lack of penetration depth, in some cases too much detail ('lose the forest for the trees'), and potentially extra equipment in the field.
机译:在过去的10年里,令人惊讶地揭示了各种各样的地貌和地质环境的地面穿透雷达(GPR)研究揭示了详细的地层信息。这些研究中的大多数是用较低频率的天线(50-100MHz)进行的,以便更好地了解地下地层。随着GPR系统和数据收集方法继续提高其收集更高质量的数字数据的能力,GPR调查旨在利用较高频率的天线进入更高分辨率探索的新时代。本文介绍了使用较高频率(225 - 900 MHz)GPR系统的四个案例研究的结果,以有效地研究沿海和Eolian沉积环境。较高频率数据的一些缺点是:缺乏穿透深度,在某些情况下,细节过多(“失去树木的森林”),以及该领域的额外设备。

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