Apart from rare metal pegmatites and granites, carbonatites and the related alkaline magmatitic rocks are the main primary source for Nb and Ta. There are many Nb-bearing minerals which may be categorized as follows and expected in carbonatites:
The major members or namesakes of each group are given and their chemical composition and contents in wt. % are shown in brackets. Rarely means more frequently in pegmatites and granites.
With kind regards
H.G.Dill
p.s. sorry for not considering the subscripts and writing it in this unconventional manner.
The Nb minerals listed by Dr. Grundmann are members of the perowskite group s.s.s. as shown above by the simplified structure (Ca, Na, LREE, Ba, Sr) (Nb, Ta, Ti, Fe)O3
Even the mineral perowskite contains moderate amounts of Nb often associated with LREE (Ce group) for charge balance reasons in carbonatites.
Loparite is among others common to the largest laccolitic alkaline magmatic complex at Lovozero, Russia,
And also the pretty rare niocalite, which is a wöhlerite-related sorosilicate in addition to all those oxides mentioned above. Nb may also occur as minor element in Ti-bearing silicates appearing in peralkaline rocks, such as titanite, melanite garnet, etc.