| 21. | The mineral occurs in nepheline syenite pegmatites and granite and aplite greisens.
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| 22. | It occurs as an alteration product of triphylite in pegmatites.
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| 23. | It has been found in association with granite pegmatite and in greisen.
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| 24. | It also occurs in skarn, pegmatite and hydrothermally altered volcanic rocks.
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| 25. | It is an accessory mineral in some tantalum-rich granite pegmatites.
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| 26. | The higher temperature pegmatites most likely preceded the hydrothermal deposits.
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| 27. | In some locations, very coarse-grained pegmatite masses occur with granite.
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| 28. | Pegmatite may be produced by low degrees of partial melting of the crust.
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| 29. | It is also found in granite pegmatites and greisens.
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| 30. | Connected with the borolanite there are other types of nepheline syenite and pegmatite.
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