高频探地雷达探测对撞击熔融角砾岩散射过程的影响——来自加拿大德文岛Haughton撞击构造北极野外活动的早期结果

T. Unrau, G. Osinski, R. Pratt, K. Tiampo
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引用次数: 3

摘要

三维探地雷达(GPR)在加拿大德文岛的Haughton撞击构造上对非均质碳酸盐为主的撞击熔融角砾岩进行了测量。选择调查地点是为了确定散射介质对行星探测中有用成像深度的影响。该测量以及相关的2D、共中点(CMP)和误差控制测量表明,尽管材料的电气适应性适合GPR,但角化单元的穿透深度比预期的要小。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The effect of scattering processes on high frequency ground penetrating radar surveys on impact melt breccia - Early results from an arctic field campaign at the Haughton impact structure, Devon Island, Canada
A 3D ground penetrating radar (GPR) survey was performed at the Haughton impact structure, Devon Island, Canada over heterogeneous carbonate-dominated impact melt breccias. The survey location was chosen for the purpose of qualifying the effect of a scattering medium on the depth of useful imaging in the context of planetary exploration. This survey, and associated 2D, common mid-point (CMP) and error control surveys, show that the depth of penetration is less on the brecciated unit than desired despite the electrical suitability of the material to GPR.
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