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首页> 外文期刊>Journal of African Earth Sciences >Seismic reflection and structuring characterization of deep aquifer system in the Dakhla syncline (Cap Bon, North-Eastern Tunisia)
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Seismic reflection and structuring characterization of deep aquifer system in the Dakhla syncline (Cap Bon, North-Eastern Tunisia)

机译:达克拉向斜向深部含水层系统的地震反射和构造特征

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摘要

The Dakhla syncline is located in the North-Eastern Tunisia. It is bounded by Abd El Rahmene anticline to the North-West, El Haouaria Graben to the North-East, Grombalia Graben to the South-West and the Mediterranean Sea to the East. The main aquifer reservoirs of Dakhla syncline are constituted by stacks of fluvial to deltaic Neogene sequences and carbonates. The interpretation of eight seismic reflection profiles, calibrated by wire line logging data of three oil wells, hydraulic wells and geologic field sections highlighted the impact of tectonics on the structuring geometry of aquifers and their distribution in elevated structures and subsurface depressions. Lithostratigraphic correlations and seismic profiles analysis through the syncline show that the principal aquifers are thickest within the central and northern part of the study area and thinnest to the southern part of the syncline.
机译:Dakhla向斜线位于突尼斯东北部。它的边界是西北部的Abd El Rahmene背斜,东北部的El Haouaria Graben,西南部的Grombalia Graben以及东部的地中海。 Dakhla向斜的主要含水层储层是由河流到三角洲的新近纪序列和碳酸盐岩堆积而成。通过对三个油井,水力井和地质现场剖面的线测井数据进行校准,对八种地震反射剖面进行了解释,突显了构造学对含水层结构几何及其在高架结构和地下凹陷中的分布的影响。通过向斜线的岩石地层相​​关性和地震剖面分析表明,主要含水层在研究区的中部和北部最厚,在向斜线的南部最薄。

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