Multi-scale hydrostructural approach for karst environment. Application to the Arcier hydrosystem (eastern France)

IF 2.6 2区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
V. Klaba , H. Celle , P. Trap , F. Choulet , L. Smeraglia , A. Malard , N. Carry
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Abstract

Based on a multi-scale and hydrostructural approach, this study presents the most relevant methodology to be applied to a karst hydrosystem in order to get a full understanding of underground water flow. It implies a complete structural analysis, from the hydrosystem scale to the outcrop scale, including the intermediate scale of the major geological structures. We illustrate the method in the Arcier hydrosystem, in the northwestern border of the Jura fold-and-thrust belt (Eastern France).

Field mapping and structural analysis allow to update the geological vision of the hydrosystem with two kink-type fault propagation folds, including a trishear kinematic model, on either side of a plateau presenting a hollow-and-dome configuration. Fracturing analysis reveals a fault-fracture network that we infer governs the entire hydrosystem. A Riedel pattern is highlighted, characterized by a N–S-striking (N355° ± 5), sinistral strike-slip, regional shear zone. Then, two 3D geological models, at different scales, constructed with MOVE and Visual Karsys softwares are combined with water levels and artificial tracer tests. It reveals a multilayer aquifer and a redefinition of groundwater circulations for the Arcier hydrosystem.

The results demonstrate a strong geological control of karstic hydrosystems on groundwater circulations, proving that classical hydrogeological methods, such as natural and/or artificial tracers, must be combined with rigorous geological analysis. Moreover, the multi-scale approach provides an explanation of groundwater circulation based on the intersection between 3D geometry of impervious layers delimiting the aquifers and their base water level, instead of the 2D view (section or map) requiring systematic recourse to inferred vertical faults to cross permeability barriers vertically or laterally. This study also brings a new vision to the local protection of the water resource.

岩溶环境的多尺度水文结构方法。应用于阿尔西耶水系(法国东部)
本研究以多尺度和水文结构方法为基础,提出了适用于岩溶水系的最相关方法,以全面了解地下水流。这意味着要进行完整的结构分析,从水系尺度到露头尺度,包括主要地质结构的中间尺度。通过实地测绘和构造分析,我们更新了该水系的地质远景,在呈现空心穹隆构造的高原两侧,有两个金克式断层扩展褶皱,包括一个三剪切运动模型。断裂分析揭示了一个断层-断裂网络,我们推断该网络控制着整个水文系统。其中突出显示了一个里德尔模式,其特征是一个北-南走向(N355° ± 5)、正弦走向滑动的区域剪切带。然后,利用 MOVE 和 Visual Karsys 软件构建的两个不同尺度的三维地质模型与水位和人工示踪试验相结合。结果表明,岩溶水文系统对地下水循环有很强的地质控制作用,证明了传统的水文地质方法,如天然和/或人工示踪剂,必须与严格的地质分析相结合。此外,多尺度方法提供了地下水循环的解释,其基础是划分含水层的不透水层的三维几何形状与其基本水位之间的交叉,而不是二维视图(剖面图或地图),后者需要系统地利用推断出的垂直断层来垂直或横向穿越渗透障碍。这项研究还为当地的水资源保护带来了新的视角。
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来源期刊
Journal of Structural Geology
Journal of Structural Geology 地学-地球科学综合
CiteScore
6.00
自引率
19.40%
发文量
192
审稿时长
15.7 weeks
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.
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