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首页> 外文期刊>Journal of Geographic Information System >Contribution of the 3D Geological Model to the Study of the High Basin Ziz Jurassic Aquifers Structure (Central High Atlas, Morocco)
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Contribution of the 3D Geological Model to the Study of the High Basin Ziz Jurassic Aquifers Structure (Central High Atlas, Morocco)

机译:3D地质模型对高盆地Ziz侏罗纪含水层结构研究的贡献(摩洛哥中部高阿特拉斯)

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摘要

The high Ziz’s basin, which is part of the Central High Atlas, contains Jurassic superficial and deep aquifers. The information sheets are still fragmentary and insufficient because of the basin’s large size and its complex geological structure. In order to improve the knowledge of these aquifers and the determination of the structure of aquifers, a 3D geological model was developed in this study. It was constructed from information provided by 200 mechanical soundings and 81 electrical surveys and geological maps. Compiled holes were analyzed, coded and integrated in the software Groundwater Modeling System 6.0 (GMS 6.0). For doing this, five lithostratigraphic units were considered: the Domerian, the Toarcian, the Aalenian, the Bajo-Bathonian and the Quaternary. The operation of the 3D stratigraphic model allowed making it closer to the geometry of Jurassic aquifers.
机译:高Ziz盆地是中央高地图集的一部分,包含侏罗纪浅层和深层含水层。由于该盆地面积大且地质结构复杂,因此信息表仍然零散且不足。为了提高对这些含水层的了解并确定含水层的结构,本研究开发了一个3D地质模型。它是由200次机械探测,81次电勘测和地质图提供的信息构造而成的。在软件“地下水建模系统6.0(GMS 6.0)”中对编译的孔进行了分析,编码和集成。为此,考虑了五个岩相地层学单位:多梅尔,托阿尔,托伦,阿伦,巴霍-巴松和第四纪。 3D地层模型的操作使其更接近侏罗纪含水层的几何形状。

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