首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >A parametric method to model 3D displacements around faults with volumetric vector fields
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A parametric method to model 3D displacements around faults with volumetric vector fields

机译:用体积矢量场对断层周围的3D位移进行建模的参数方法

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This paper presents a 3D parametric fault representation for modeling the displacement field associated with faults in accordance with their geometry. The displacements are modeled in a canonical fault space where the near-field displacement is defined by a small set of parameters consisting of the maximum displacement amplitude and the profiles of attenuation in the surrounding space. The particular geometry and the orientation of the slip of each fault are then taken into account by mapping the actual fault onto its canonical representation. This mapping is obtained with the help of a curvilinear frame aligned both on the fault surface and slip direction.This formulation helps us to include more geological concepts in quantitative subsurface models during 3D structural modeling tasks. Its applicability is demonstrated in the framework of forward modeling and stochastic sequential fault simulations, and the results of our model are compared to observations of natural objects described in the literature.
机译:本文提出了一种3D参数故障表示法,用于根据故障的几何形状对与故障关联的位移场进行建模。在规范的断层空间中对位移进行建模,在该区域中,近场位移由一小组参数定义,该参数集由最大位移幅度和周围空间的衰减曲线组成。然后,通过将实际断层映射到其规范表示中,来考虑每个断层的特定几何形状和滑动方向。通过在断层表面和滑动方向上均对齐的曲线框架获得此映射。此公式可帮助我们在3D结构建模任务期间将更多地质概念纳入定量地下模型中。在正演建模和随机顺序故障模拟的框架中证明了其适用性,并将我们的模型结果与文献中描述的自然物体的观测结果进行了比较。

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