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The Tinguicht pluton is part of the ∼2.07 Ga post-collisional magmatic suites that intruded the Yetti Paleoproterozoic volcano-sedimentary series of the western part of the Eglab Shield (West African Craton). It represents one of the most recent units of these suites. This pluton, with a NW–SE elliptic shape, is unfoliated, and its deformational structures are practically restricted to fracturing...
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