Continental margin subsidence from shallow mantle convection: Example from West Africa

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Continental margin subsidence from shallow mantle convection: Example from West Africa

Spatial and temporal evolution of the uppermost convecting mantle plays an important role in determining histories of magmatism, uplift, subsidence, erosion and deposition of sedimentary rock. Tomographic studies and mantle flow models suggest that changes in lithospheric thickness can focus convect...

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Bibliographic Details
Main Authors:	Lodhia, Bhavik, Roberts, G.G., Fraser, A.J., Fishwick, S., Goes, S., Jarvis, J.
Format:	Journal Article
Published:	2018
Online Access:	http://hdl.handle.net/20.500.11937/97476

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