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.

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oai:nora.nerc.ac.uk:13769

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

Authors: B. Bingen
G. Viola
R. Boyd
R.J. Thomas
J. Jacobs
I.H.C. Henderson
Ø. Nordgulen
J.S. Sandstad
A.K. Engvik
M. Smethurst
Ø. Skar
A. Solli
R.M. Key
E.X. Daudi
Publication date: 1 January 2011
Publisher: Geological Society of Africa

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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oai:nora.nerc.ac.uk:13769

Last time updated on 03/07/2012

This paper was published in NERC Open Research Archive.

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