| 1. | Biotite, cancrinite and sodalite are characteristic of this rock.
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| 2. | Nepheline generally shows partial alteration into natrolite and cancrinite.
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| 3. | It is essentially a microcline, sodalite and cancrinite variety of nepheline syenite.
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| 4. | Sodalite transforms into cancrinite when exposed to high temperature.
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| 5. | The mineral of cancrinite is named after him.
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| 6. | Cancrinite occurs in several nepheline-syenites.
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| 7. | Bystrite has a structure that is shared with many of the minerals in the cancrinite group.
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| 8. | It is associated with other minerals typical of undersaturated environments, namely leucite, cancrinite and natrolite.
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| 9. | Nepheline is very abundant and there is also cancrinite, sodalite, scapolite, calcite, biotite and hornblende.
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| 10. | In high temperature, sodalite would transform to cancrinite of which twelve-ring channels cage prefer bigger cation.
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