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首页> 外文期刊>Journal of African Earth Sciences >Contribution of gravity and aeromagnetic data to the structural modeling of the hidden faults in Guercif Basin, northeastern Morocco
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Contribution of gravity and aeromagnetic data to the structural modeling of the hidden faults in Guercif Basin, northeastern Morocco

机译:重力和航磁数据对摩洛哥东北部Guercif盆地隐伏断层的结构模拟的贡献

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摘要

The Guercif Basin of the northeastern Morocco is regarded as a particular sedimentary basin influenced by the tectonics of the Middle Atlas Fault Zone, the Rif orogenic belt and the stable eastern Meseta. Its faulting structures are poorly perceived on surface because of the thick recent sedimentary cover that overlies the Mesozoic-Paleozoic basement. The interpretation of potential field data shows relevant results in deciphering the basement structure of a complex sedimentary basin, such as the Guercif Basin. In order to understand the structural framework of this basin and to establish its subsurface structural map, gravity and magnetic data were processed using various edge detection techniques accomplished by an extensive geological data and seismic interpretations.A new subsurface structural map was established where many faults already recognized or supposed by traditional structural studies have been confirmed and new major ones by specifying their trends and depths have been emphasized. In addition, this new map demonstrates that the Guercif Basin is affected by several major faults elongated in three main trends: NE-SW, E-W and NW-SE, inherited from Variscan tectonics and reactivated in relation with atlasico-alpine tectonics.The established referential map reveals that the study area is subdivided into two different structural domains; a western one principally affected by NE-SW trending faults representing the northeastern extension of the Middle Atlas Fault Zone, and an eastern domain belonging to the stable eastern Meseta and characterized in general by large E-W trending faults. It allows us also to identify a sinistral fault zone in Tafrata area which we have labeled "Tafrata Fault Zone" and to define the continuity of the North Middle Atlas Fault (NMAF), the Central Middle Atlas Faults (CMAF) and the South Middle Atlas Fault (SMAF) which presents very likely the limit between the two identified domains. The elaborated map will be a useful document for all future petroleum explorations or hydrogeological investigations.
机译:摩洛哥东北部的Guercif盆地被视为受中阿特拉斯断层带,Rif造山带和稳定的Meseta东部构造影响的特殊沉积盆地。由于中生代-古生代基底上覆盖着较厚的近期沉积层,因此在地表上很难看到其断层结构。对潜在场数据的解释显示了在解密复杂的沉积盆地(例如Guercif盆地)的基底结构方面的相关结果。为了了解该盆地的构造框架并建立其地下构造图,利用广泛的地质数据和地震解释所完成的各种边缘检测技术对重力和磁数据进行了处理。已经确认了传统结构研究认可或假定的特征,并强调了通过指明其趋势和深度的新的主要研究。此外,这张新地图还显示了Guercif盆地受到几个主要断层的影响,这些断层在三个主要趋势上延伸:NE-SW,EW和NW-SE,这些断层是从瓦里斯坎构造继承而来的,并与Atlasico-Alpine构造有关。地图显示研究区域被细分为两个不同的结构域;西部主要受NE-SW趋势断层影响,代表中阿特拉斯断层带的东北延伸,而东部地区属于稳定的Meseta东部,通常以大型E-W趋势断层为特征。它也使我们能够识别出我们已标记为“塔弗拉塔断层带”的塔弗拉塔地区的左旋断裂带,并定义了北中阿特拉斯断层(NMAF),中中阿特拉斯断层(CMAF)和南中阿特拉斯的连续性故障(SMAF)很有可能在两个确定的域之间提供限制。精心制作的地图将是将来所有石油勘探或水文地质调查的有用文件。

著录项

  • 来源
    《Journal of African Earth Sciences》 |2020年第4期|103797.1-103797.19|共19页
  • 作者

  • 作者单位

    Moulay Ismail Univ Fac Sci Dept Earth Sci BP 11201 Zitoune Meknes Morocco;

    Ibn Tofail Univ Fac Sci Dept Earth Sci Kenitra Morocco;

    Hassan II Univ Fac Sci Ain Chock Dept Earth Sci BP 5366 Casablanca Morocco;

    Univ Tunis El Manar Fac Sci Tunis Tunis 1060 Tunisia;

    Minist Energy Mines & Sustainable Dev Directorate Geol Rabat Morocco;

    Univ Mohammed V Rabat Ctr Rech Geophys Nat Patrimony & Green Chem GEOPA Inst Sci Rabat Morocco;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Gravimetry; Aeromagnetism; Hidden faults; Tectonic blocks; Alpine evolution; Guercif basin; Northeastern Morocco;

    机译:重量分析航空磁性隐藏的故障;构造块体高山演化;格尔西夫盆地;摩洛哥东北部;

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