Article ID Journal Published Year Pages File Type
6443837 Journal of African Earth Sciences 2014 13 Pages PDF
Abstract
It is suggested that the alkaline to calc-alkaline volcanic transition reflects the evolution of the Francevillian basin from a diverging to a converging setting, in response to the onset of converging movements in the Eburnean Belt of Central Africa.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
Authors
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