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The Oka carbonatite complex, one of the Cretaceous Monteregian Hills intrusions, consist of a wide range of silicate and carbonatite rocks (e.g. sovite, urtite, ijolite, jacupirangite, okaite). In the 60s, due to the abundance of pyrochlores and Nb-bearing perovskites, niobium mine (St. Lawrence Columbium mine) was developed and active until its closure in 1977, however significant amount of niobium minerals still remain at the deposit and surrounding dumps. Besides economic value as a niobium ore (and potentially...