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Understanding the tectonic setting of northern-eastern Mozambique is crucial for evaluating<br>precise reconstruction of central Gondwana. Mozambiquean (1.0 – 1.2 Ga) and Pan-African (0.5-0.7<br>Ga) orogenic events have been recognized in this region that may well contain remnants of older<br>crustal material (Pinna et al., 1993; Kröner et al 1997 and Jamal, et al., 1999).