Lower Cretaceous alkaline-carbonatite complex (10 km diameter) in Precambrian granito-gneissic basement.
Carbonatite ring, rimmed to the east by fenitized ijolites, within nepheline syenite body.
Younger alkali gabbro/syenite intrusion.
References:
-Mariano, A. N., Roeder, P. L., 1989. Wöhlerite: chemical composition, cathodoluminescence and environment of crystallization. Canadian Mineralogist, 27: 709-720.
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