Identification of potential mineral exploration targets from the interpretation of aeromagnetic data covering the Sirwa region (Central Anti-Atlas, Morocco)

被引:3
|
作者
Tazi, Mohammed Jalal [1 ]
El Azzab, Driss [1 ]
Charroud, Mohammed [1 ]
Jabrane, Oussama [1 ]
Ouahzizi, Youssef [1 ]
Zahour, Rachid [1 ]
Amadou, Abdourahamane Halidou [1 ]
机构
[1] Sidi Mohamed Ben Abdellah Univ, Fac Sci & Technol, SIGER Lab, BP2202, Fes, Morocco
关键词
Aeromagnetic data; Edge detection techniques; Hidden faults; Sirwa; Anti-atlas; Morocco; WEST-AFRICAN CRATON; NEOPROTEROZOIC EPITHERMAL MINERALIZATION; LITHOSTRATIGRAPHIC FRAMEWORK; PASSIVE MARGIN; SIROUA; INLIER; TECTONICS; BASEMENT; GEOCHEMISTRY; DEPOSIT;
D O I
10.1016/j.sciaf.2022.e01351
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Situated at the junction between the Moroccan High Atlas and the Anti-Atlas, the Sirwa Massif has always been a perfect target for mining exploration for its unique geological characteristics that provide an economically valuable concentrations of metals. It corre-sponds to a crustal uplift at an elevation above 20 0 0 m that were slightly folded and lifted during the Hercynian and Alpine orogeny. The structural settings of this area are very complicated due to the acute shortage of surface and subsurface structural data. The aeromagnetic data represents a powerful tool for the identification and the delineation of the poorly exposed faults, that could promote the development of new ore deposits.The processing of the residual magnetic map was carried out to locate anomalies, de-fine the trends and boundaries of the buried structures and identify the magnetic con-tacts that might represent faults, fractures or lithologic boundaries. This is done by the reduction to the north pole (RTP) filter and several edge detectors processes (i.e., total horizontal derivative, the tilt angle derivative and the 3D-Euler deconvolution). The ori-entations of lineaments extracted from the total horizontal derivative and Tilt derivative maps predominantly suggest NE-SW to ENE-WSW trending structures, in agreement with the post-Pan-African rifting event. However, we have identified a few NW-SE and NNW -SSE trending lineaments probably related to the recent Variscan movements. The 3D Eu-ler deconvolution (ED) suggests a depth solution that ranges from 600 m to 3400 m. The deepest lineaments have an ENE-WSW direction, and the shallowest with a depth of about 600 m, shows a NE-SW/NW-SE direction. These results reveal new tectonic features that can be useful for future mine exploration (c) 2022 The Authors. Published by Elsevier B.V. on behalf of African Institute of Mathematical Sciences / Next Einstein Initiative.This is an open access article under the CC BY-NC-ND license ( http://creativecommons.org/licenses/by-nc-nd/4.0/ )
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页数:13
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