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首页> 外文期刊>Geosphere >Quantitative analysis and visualization of nonplanar fault surfaces using terrestrial laser scanning (LIDAR)--The Arkitsa fault, central Greece, as a case study
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Quantitative analysis and visualization of nonplanar fault surfaces using terrestrial laser scanning (LIDAR)--The Arkitsa fault, central Greece, as a case study

机译:使用地面激光扫描(LIDAR)对非平面断层表面进行定量分析和可视化-以希腊中部的Arkitsa断层为例

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摘要

Many fault surfaces are noticeably nonplanar, often containing irregular asperities and more regular corrugations and open warping. Terrestrial laser scanning (light detection and ranging, LIDAR) is a powerful and versatile tool that is highly suitable for acquisition of very detailed, precise measurements of slip-surface geometry from well-exposed faults. Quantitative analysis of the LIDAR data, combined with three-dimensional visualization software, allows the spatial variation in various geometrical properties across the fault surface to be clearly shown. Plotting the variation in distance of points from the mean fault plane is an effective way to identify culminations and depressions on the fault surface. Plots showing the spatial variation of surface orientation are useful in highlighting corrugations and warps of different wavelengths, as well as cross faults and fault bifurcations. Analysis of different curvature properties, including normal and Gaussian curvature, provides the best plots for quantitative measurements of the geometry of corrugations and folds. However, curvature analysis is highly scale dependent, so requires careful filtering and smoothing of the data to be able to analyze structures at a given wavelength.
机译:许多断层表面明显是非平面的,通常包含 不规则的凹凸,以及更规则的波纹和开放的 翘曲。地面激光扫描(光检测和测距, LIDAR)是一种功能强大且用途广泛的工具,非常适合 用于获取非常详细,精确的滑动表面测量 来自暴露良好的断层的几何。对 LIDAR数据的定量分析,结合三维可视化 软件,可以确定整个断层表面各种几何 属性的空间变化。清楚显示。绘制 点到平均断层平面的距离变化 是识别断层表面上的高点和凹陷的有效方法。显示 表面方向的空间变化的图对于突出波纹 和不同波长的翘曲以及交叉断层 和断层分叉非常有用。对不同曲率特性(包括法向曲率和高斯曲率)的分析提供了用于定量测量波纹 和褶皱的最佳图 。但是,曲率分析高度依赖于比例, 因此需要仔细过滤和平滑数据,以便 能够分析给定波长下的结构。

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  • 来源
    《Geosphere》 |2009年第6期|465-482|共18页
  • 作者单位

    Geospatial Research Ltd., Department of Earth Sciences, University of Durham, Durham DH1 3LE, UK|Reactivation Research Group, Department of Earth Sciences, University of Durham, Durham DH1 3LE, UK;

    University of Patras, Department of Geology, Laboratory of Structural Geology, 26500 Patras, Greece;

    Reactivation Research Group, Department of Earth Sciences, University of Durham, Durham DH1 3LE, UK;

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