Arid
DOI10.1016/j.jafrearsci.2022.104581
Gravity study of the Western Bahira Basin and the Gantour Phosphatic Plateau, central Morocco: Interpretation and hydrogeological implications
Jaffal, Mohammed; Charbaoui, Anas; Kchikach, Azzouz; El Ghorfi, Mustapha; Khaldoun, Abdelhadi; Safhi, Amine El Mahdi; Bodinier, Jean-Louis; Yazami, Oussama Khadiri; Jourani, Es-Said; Manar, Ahmed
通讯作者Jaffal, M
来源期刊JOURNAL OF AFRICAN EARTH SCIENCES
ISSN1464-343X
EISSN1879-1956
出版年2022
卷号193
英文摘要The Western Bahira Basin (WBB), located in Central Morocco, is known for its large reserves of phosphate, which are currently being extracted through open pit mines within the Gantour Phosphatic Plateau (GPP). This mining activity, as well as the increasing agricultural development that this region has been experiencing during the last few decades, has subjected the groundwater in this semi-arid region to intense exploitation through pumping. Consequently, thorough knowledge of the underground water resources is essential for sustained activity.This study uses gravity data to investigate the deep geologic structure of the western Bahira and Gantour plateau area. Its main purpose is to improve the knowledge of this structure that influences the groundwater dynamics.The methodology involves, in addition to the qualitative and quantitative interpretation of the gravity data, the use of various filtering and analysis techniques to highlight the major geological structures. In fact, a qualitative analysis of the residual gravity map shows that the observed anomalies can be explained in terms of the bedrock topography of the study area. Positive anomalies spatially correlate with the outcrops of this bedrock in the Hercynian massifs of Jebilet and Rehamna, as well as with the Douar Rhirat structural high. The negative anomalies, on the other hand, tend to reflect increased thicknesses of sedimentary sequences, such as in the southern part of the WBB. Moreover, the Brikyine granite in the north of the study area is noticeably associated with the highest amplitude negative anomaly.Analysis of the residual gravity data using the total horizontal gradient, upward continuation, and Euler deconvolution techniques provides a quantitative assessment of the geologic structure. These methods help delineate various structures oriented in two main directions: N45E and N105E. Among these structures, several major faults have been identified. They are rooted at a maximum depth in excess of 2800 m. These faults are responsible for the general structure of the study area and the morphology of the basement. Furthermore, the 2D forward modeling, performed across the main negative gravity anomalies of the WBB, helps characterize the Paleozoic bedrock topography and provides more constraints on its variation. The resultant gravity models clearly show an asymmetric structure for the western Bahira trough. This depression is filled by sedimentary formations whose thickness at the depot-center can locally reach 1200 m. Additional analysis of piezometric data shows that the groundwater flows are controlled by the gravity structures high-lighted in this study.
英文关键词Gravity filtering Structure Hydrogeology Western bahira basin Gantour phosphatic plateau Morocco
类型Article
语种英语
开放获取类型Green Submitted
收录类别SCI-E
WOS记录号WOS:000805938800002
WOS关键词EULER ; GRAVIMETRY ; DEPTH
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/393264
推荐引用方式
GB/T 7714
Jaffal, Mohammed,Charbaoui, Anas,Kchikach, Azzouz,et al. Gravity study of the Western Bahira Basin and the Gantour Phosphatic Plateau, central Morocco: Interpretation and hydrogeological implications[J],2022,193.
APA Jaffal, Mohammed.,Charbaoui, Anas.,Kchikach, Azzouz.,El Ghorfi, Mustapha.,Khaldoun, Abdelhadi.,...&Manar, Ahmed.(2022).Gravity study of the Western Bahira Basin and the Gantour Phosphatic Plateau, central Morocco: Interpretation and hydrogeological implications.JOURNAL OF AFRICAN EARTH SCIENCES,193.
MLA Jaffal, Mohammed,et al."Gravity study of the Western Bahira Basin and the Gantour Phosphatic Plateau, central Morocco: Interpretation and hydrogeological implications".JOURNAL OF AFRICAN EARTH SCIENCES 193(2022).
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