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The Use of Ground Penetrating Radar for Mapping Rock Stratigraphy and Tectonics:Implications for Geotechnical Engineering

The Use of Ground Penetrating Radar for Mapping Rock Stratigraphy and Tectonics:Implications for Geotechnical Engineering

作     者:Awni T Batayneh Taisser Zumlot Habes Ghrefat Mahmud M El-Waheidi Yousef Nazzal 

作者机构:Department of Geology and Geophysics King Saud UniversityPO Box 2455 Riyadh 11451 Saudi Arabia 

出 版 物:《Journal of Earth Science》 (地球科学学刊(英文版))

年 卷 期:2014年第25卷第5期

页      面:895-900页

核心收录:

学科分类:070904[理学-构造地质学] 081801[工学-矿产普查与勘探] 081802[工学-地球探测与信息技术] 0709[理学-地质学] 07[理学] 08[工学] 0708[理学-地球物理学] 0818[工学-地质资源与地质工程] 0704[理学-天文学] 

基  金:extend their sincere appreciation to the Deanship of Scientific Research at King Saud University for its funding this research work sincerely a support received from the Natural Resources Authority of Jordan to accomplish this work 

主  题:ground penetrating radar rock stratigraphy rock tectonics Ras en Naqab Jordan. 

摘      要:This paper presents results from ground penetrating radar surveys using the SIR-10 B GPR instrument(manufactured by Geophysical Survey System Inc., USA), with 400 MHz monostatic antenna(model 5 103). Survey was made over 3 excavation levels along the highway section at the Ras en Naqab escarpment area, Southwest Jordan. A total of 217 m along 4 profiles were covered in the winter of 2012. The objectives of the study are(i) to evaluate the resolution of the GPR technique in the field for detecting and locating anomalies caused by subsurface structures like cavities, fractures and faults, and(ii) to describe stratigraphic nomenclature of the subsurface rocks of the area. 2D interpretation of the obtained data and the geological information demonstrate a strong correlation between the GPR anomalies and the subsurface geology. Based upon the lateral and vertical velocity changes with depth, the thickness and orientation of the subsurface layers are outlined. Analysis of the exposed section shows good agreement between the estimated thicknesses of lithostratigraphic units and the quantitative assessment of the radar waves velocity inferred from GPR data.

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