Review paper
Intracontinental anorogenic alkaline magmatism and carbonatites, associated mineral systems and the mantle plume connection
Abstract
Intracontinental alkaline complexes and carbonatites commonly occur in rift-related settings, best exemplified by the Cenozoic–present day East African Rift System. Examples in the ancient geological record are more difficult to unravel due to subsequent overprinting during tectono-thermal events unrelated to the original rifting. In the present paper, with the exception of the Bayan Obo carbonatite, I have used examples of anorogenic alkaline...
Paper Details
Title
Intracontinental anorogenic alkaline magmatism and carbonatites, associated mineral systems and the mantle plume connection
Published Date
Apr 1, 2015
Journal
Volume
27
Issue
3
Pages
1181 - 1216
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