Gloria Arienti , Andrea Bistacchi , Guillaume Caumon , Bruno Monopoli , Giovanni Dal Piaz
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引用次数: 0
摘要
我们提出了一个建模工作流程,用于创建在意大利奔宁阿尔卑斯山脉内的Lago di Cignana地区暴露的构造建筑的公里尺度的三维表示。该模型描绘了显著的构造边界,如登特-布兰奇基底逆冲、组合断裂和罗桑-奇尼亚纳剪切带。我们的方法采用隐式离散平滑插值器,它将构造序列表示为一个推广相对距离函数的体积标量场。插值过程受到地质和构造野外资料的限制。为了模拟在该区域露头的褶皱,我们对褶皱轴进行三维插值,并通过在最小二乘系统中补充正则化项的切线约束,在褶皱几何形状上强制执行这些插值方向。此外,我们通过模拟随机位置露头的虚拟数据集合和随机模拟远离直接观测的褶皱轴来解决该地区暴露的等斜平卧褶皱的结构不确定性。这些模拟的褶皱轴以与现场数据一致的球形方向分布排列,并用作隐式插值的附加约束。不确定性分析在轴向和肢间角方面产生了非圆柱形褶皱的多种情况。
3D structural implicit modelling of folded metamorphic units at Lago di Cignana with uncertainty assessment
We present a modelling workflow for the creation of a km-scale, three-dimensional representation of the tectonic architecture exposed in the Lago di Cignana region within the Italian Pennine Alps. The model portrays notable tectonic boundaries such as the Dent Blanche Basal Thrust, the Combin Fault and the Roisan-Cignana Shear Zone. Our approach employs the implicit Discrete Smooth Interpolator, which represents the tectonic sequence as a volumetric scalar field generalising a relative distance function. The interpolation process is constrained by geological and structural field data. To model folds that outcrop in the region, we perform three-dimensional interpolation of fold axes, and we enforce these interpolated directions on the fold geometries through tangent constraints complementing the regularisation term in the least-squares system. Furthermore, we address structural uncertainty on isoclinal recumbent folds exposed in the area by simulating a collection of virtual data at randomly located outcrops and stochastically simulating fold axes away from direct observations. These simulated fold axes are arranged in spherical orientation distributions consistent with field data and are used as additional constraints for implicit interpolation. The uncertainty analysis generates multiple scenarios for non-cylindrical folds in terms of axis orientations and interlimb angle.
期刊介绍:
The Journal of Structural Geology publishes process-oriented investigations about structural geology using appropriate combinations of analog and digital field data, seismic reflection data, satellite-derived data, geometric analysis, kinematic analysis, laboratory experiments, computer visualizations, and analogue or numerical modelling on all scales. Contributions are encouraged to draw perspectives from rheology, rock mechanics, geophysics,metamorphism, sedimentology, petroleum geology, economic geology, geodynamics, planetary geology, tectonics and neotectonics to provide a more powerful understanding of deformation processes and systems. Given the visual nature of the discipline, supplementary materials that portray the data and analysis in 3-D or quasi 3-D manners, including the use of videos, and/or graphical abstracts can significantly strengthen the impact of contributions.