Delineation of subsurface structures using gravity interpretation around Nabaa Al Hammara area, Wadi El Natrun, Egypt

Mahmoud S. Awad, Hassan H. El Kadi, A. M. Abbas, Sultan Awad Sultan Araffa
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Abstract

ABSTRACT Nabaa El Hammra lies in the northeastern part of Wadi El-Natrun, characterised by low lands and most parts of this area are cultivated with different crops. In the current study, gravity data are used to investigate the subsurface structural features that can directly affect the configuration and distribution of groundwater aquifers and oil reservoirs accumulations. The present study aims to delineate the subsurface structural elements and to define the basins and basement uplifts, which can directly affect the flow of groundwater or oil accumulations. Gravity data are processed and filtered in diverse approaches to outlining the prevailed structure. The results of gravity data interpretation reveal that the studied area is affected by many structural features as NE-SW, NW-SE, N-S and E-W trends. These structural features caused barriers to the groundwater movement from or to the study area. The study revealed that the depth of the crystalline (Pre-Cambrian) rocks ranges from 3800 metres in the south part to 5300 metres in the northeastern region. Meanwhile, the basement rocks represent a bridge of shallow depth of northwest-southeast trend at the centre of the investigated area.
利用重力解释描绘埃及Wadi El Natrun地区Nabaa Al Hammara地区的地下结构
纳巴哈姆拉(Nabaa El Hammra)位于瓦迪纳特伦(Wadi El- natrun)的东北部,地势低洼,大部分地区种植着不同的作物。在本研究中,重力数据被用于研究直接影响地下水含水层形态和分布以及油藏聚集的地下构造特征。本研究旨在圈定地下构造要素,明确直接影响地下水流动或油气聚集的盆地和基底隆升。重力数据以不同的方法进行处理和过滤,以概述普遍的结构。重力资料解释结果表明,研究区受NE-SW、NW-SE、N-S和E-W等多种构造特征的影响。这些构造特征对地下水进出研究区造成了障碍。研究结果表明,结晶(前寒武纪)岩石的深度从南部的3800米到东北部的5300米不等。同时,基岩在研究区中心呈西北—东南走向的浅深度桥状。
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