What is a nepheline syenite in geology ?
Nepheline syenite : definition
It is a highly undersaturated grainy igneous rock, consisting mainly of alkali feldspars, usually perthitic microcline (on average 70%), and feldspathoids (mainly nepheline, more rarely sodalite, analcime or hauyne (on average 20 %), biotite, amphibole (riebeckite) and pyroxene like aegirine, sometimes cancrinite. Apatite, titanite, zircon, fluorite and sometimes calcite, corundum and eudialyte are abundant, defining many varieties and allowing the exploitation of these rocks as ore of zirconium, rare earth elements or phosphorus.
Nepheline syenites draw small intrusive massifs associated with syenites, carbonatites or peridotites. Pegmatitic facies with large crystals, called pegmatitoids, frequently line the edges. Their volcanic equivalent is the phonolite.
Nepheline syenites draw small intrusive massifs associated with syenites, carbonatites or peridotites. Pegmatitic facies with large crystals, called pegmatitoids, frequently line the edges. Their volcanic equivalent is the phonolite.
The most famous deposits are those of the Kola Peninsula (Russia), Illimaussaq (Greenland) and the Arendal region (Norway).
Eudialyte from Russia
Eudialyte from Russia