Orogenic decay from collision to rifting – characteristics and implications of delamination illustrated by a case study of the East African-Antarctic Orogen in NE Mozambique

Ueda, Kosuke

Ueda, Kosuke

Doctoral thesis

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Paper IV: Accepted version. (5.992Mb)

URI

https://hdl.handle.net/1956/4616

Date

2011-03-11

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Department of Earth Science [629]

Has parts

Paper I: Precambrian Research 178(1-4), Thomas, R. J.; Jacobs, J.; Horstwood, M. S. A.; Ueda, K.; Bingen, B.; Matola, R., The Mecúburi and Alto Benfica Groups, NE Mozambique: Aids to unravelling ca. 1 and 0.5 Ga events in the East African Orogen, pp. 72-90. Published version. Copyright © 2010 Elsevier B.V. All rights reserved. Full text not available in BORA. The published version is available at: http://dx.doi.org/10.1016/j.precamres.2010.01.010

Paper II: Ueda, K.; Jacobs, J.; Thomas, R. J.; Kosler, J.; Jourdan, F.; Matola R., Delamination-induced late tectonic deformation and high-grade metamorphism of the Proterozoic Nampula Complex, northern Mozambique. Submitted version. Submitted to Precambrian Research, Precam-3013. Full text not available in BORA.

Paper III: Ueda, K.; Jacobs, J.; Thomas, R. J.; Kosler, J.; Jourdan, F.; Horstwood, M. S. A.; Kumar, R.; Matola R., Post-collisional high-grade metamorphism, orogenic collapse, and differential cooling in NE Mozambique. Draft version. In preparation. Full text not available in BORA.

Paper IV: Tectonics 30, TC2002, Emmel, B.; Kumar, R.; Ueda, K.; Jacobs, J.; Daszinnies, M.; Thomas, R. J.; Matola R., Thermochronological history of an orogen-passive margin system - an example from N Mozambique. Accepted version. Copyright 2011 American Geophysical Union. All Rights Reserved. The published version is available at: http://dx.doi.org/10.1029/2010TC002714

Paper V: Ueda, K.; Gerya, T. V., Early convergence controls and implications of orogenic delamination. Draft version. In preparation. Full text not available in BORA.

Paper VI: Ueda, K.; Jacobs, J.; Gerya, T. V.; Thomas, R. J.; Emmel, B., Slow digestion of the jelly sandwich – the late break-up of weak continents after orogenic delamination. Draft version. In preparation. Full text not available in BORA.

Publisher

The University of Bergen