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Geological evolution of Northeastern Mozambique, in the context of the Pan-African Gondwana assembly

Bingen, B.; Viola, G.; Boyd, R.; Thomas, R.J.; Jacobs, J.; Henderson, I.H.C.; Nordgulen, Ø.; Sandstad, J.S.; Engvik, A.K.; Smethurst, M.; Skar, Ø.; Solli, A.; Key, R.M.; Daudi, E.X.. 2011 Geological evolution of Northeastern Mozambique, in the context of the Pan-African Gondwana assembly. In: 23rd Colloquium of African Geology, Johannesburg, South Africa, 8-14 Jan 2011. Geological Society of Africa, 46. (Unpublished)

Abstract
Results of an integrated geological mapping, geochronological, geochemical and airborne geophysics programme in NE Mozambique bring improved constraints on the sequence of events leading to the assembly of Gondwana along the East African Orogen (see Reference List). From the NW (foreland) to the SE (hinterland), a crustal transect across NE Mozambique shows division into 4 major lithotectonic units.
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