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Using integrated near-surface geophysical surveys to aid mapping and interpretation of geology in an alluvial landscape within a 3D soil-geology framework

机译:利用综合近地表地球物理调查,帮助在三维土壤 - 地质框架内的冲积景观中绘制地质图并进行解释

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摘要

An integrated geological, geophysical and remote sensing survey was undertaken as part of the construction of a high-resolution 3D model of the shallow subsurface geology of part of the Trent Valley in Nottinghamshire, UK. The 3D model was created using the GSI3D software package and the geophysical techniques used included ground-penetrating radar (GPR), electrical resistivity tomography (ERT) and automated resistivity profiling. In addition, the remote sensing techniques of light detection and ranging (LIDAR) and airborne thematic mapping (ATM) were used. The objective of the study was to assess the contribution of these techniques to improve the geological mapping and interpretation of terrace deposits and other geological features. The study site had an area of ~2 km2 and consisted of a Triassic mudstone escarpment, overlain first by a sand and gravel river terrace that extended to the modern floodplain of the River Trent. Automated resistivity profiling mapping proved to be the central tool in identifying and positioning geological features at a greater resolution than would be obtained through traditional geological mapping and borehole observation. These features included i) a buried cliff delineating the south-eastern limits of the incised Trent valley, ii) siltstone beds within the Gunthorpe Member of the Mercia Mudstone Group and iii) the variability of the sediments within the river terrace. A long ERT transect across the site successfully imaged the buried cliff and outcropping siltstone beds on the escarpment. Combined ERT and GPR transects revealed the depth of the sand and gravel deposits (Holme Pierrepont sands and gravels), whilst the GPR provided information about the depositional environment. Remote sensing using light detection and ranging proved essential in the original geological survey because it confirmed the absence of a second river terrace that had been previously thought to exist. This case study demonstrates the importance of combining geophysical techniques with traditional geological survey and borehole analysis, in order to create high-resolution 3D geological models, which are increasingly being used as a platform to understand and solve environmental problems.
机译:作为英国诺丁汉郡特伦特河谷部分浅层地下地质高分辨率3D模型构建的一部分,进行了综合的地质,地球物理和遥感勘测。使用GSI3D软件包创建了3D模型,使用的地球物理技术包括探地雷达(GPR),电阻率层析成像(ERT)和自动电阻率分析。此外,还使用了光探测与测距(LIDAR)和机载专题制图(ATM)的遥感技术。这项研究的目的是评估这些技术对改善地质绘图和阶地沉积物及其他地质特征的贡献。研究地点面积约2平方公里,由三叠纪泥岩悬崖组成,首先覆盖在沙砾河阶地上,并延伸至特伦特河的现代洪泛区。事实证明,自动电阻率剖面图是识别和定位地质特征的主要工具,其分辨率要比传统地质图和钻孔观测获得的分辨率更高。这些特征包括:i)划定的特伦特山谷东南边界的掩埋悬崖; ii)梅西娅泥岩群的贡索普成员内的粉砂岩层; iii)河阶地内沉积物的变化性。穿过该站点的长ERT断面成功地拍摄了悬崖上的掩埋悬崖和露头粉砂岩床的图像。结合的ERT和GPR断面揭示了沙子和砾石沉积物的深度(Holme Pierrepont沙子和砾石),而GPR提供了有关沉积环境的信息。在原始的地质调查中,使用光检测和测距进行的遥感被证明是必不可少的,因为它证实了先前认为没有的第二条河阶地的存在。该案例研究证明了将地球物理技术与传统地质调查和井眼分析相结合的重要性,以创建高分辨率的3D地质模型,这些模型正越来越多地用作理解和解决环境问题的平台。

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