What is the tectonic setting of the Bou Azzer inlier?
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The Bou Azzer inlier is located in the central part of the Anti-Atlas chain, which is on the northern margin of the West African Craton . It is characterized by a complex tectonic history and is part of the Pan-African orogenic belt . The region has experienced multiple tectonothermal events, including the obduction of supra-subduction ophiolite and oceanic arc material, the development and closure of a wide marginal basin, and post-collisional magmatism . The Bou Azzer inlier is structurally controlled by faults, with two main types of faults controlling the mineralization in the F53 vein deposit . The regional stress field in the Bou Azzer inlier is characterized by a horizontal compression tectonic regime, with a main compressive stress direction of N°30 . The granitoids in the Bou Azzer inlier have geochemical features of volcanic arc magmas and were emplaced during a major magmatic event between 640 and 660 Ma . Overall, the tectonic setting of the Bou Azzer inlier is complex, with a history of obduction, basin development, and post-collisional magmatism.
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25 Sep 2019 2 Citations | The tectonic setting of the Bou Azzer inlier is not mentioned in the provided paper. |
1 Citations | The tectonic setting of the Bou Azzer inlier is characterized by a horizontal compression tectonic regime, as indicated by several systems of strike-slip faults with a high tendency to deformation. |
| The tectonic setting of the Bou Azzer inlier in the Anti-Atlas Pan-African belt is still under debate and not clearly mentioned in the provided paper. | |
| The tectonic setting of the Bou Azzer inlier is located in the central part of the Anti-Atlas, which is on the northern margin of the West African craton. |
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