Nephelinite

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Nephelinite lava (grey) containing a xenolith of peridotite (yellow), Kaiserstuhl, Germany.

Nephelinite is a fine-grained or

clinopyroxene (variety augite). If olivine is present, the rock may be classified as an olivine nephelinite. Nephelinite is dark in color and may resemble basalt in hand specimen. However, basalt consists mostly of clinopyroxene (augite) and calcic plagioclase
.

Basalt, alkali basalt, basanite, tephritic nephelinite, and nephelinite differ partly in the relative proportions of plagioclase and nepheline. Alkali basalt may contain minor nepheline and does contain nepheline in its CIPW normative mineralogy. A critical ratio in the classification of these rocks is the ratio nepheline/(nepheline plus plagioclase). Basanite has a value of this ratio between 0.1 and 0.6 and also contains more than 10% olivine. Tephritic nephelinite has a value between 0.6 and 0.9. Nephelinite has a value greater than 0.9. Le Maitre (2002) defines and discusses these and other criteria in the classification of igneous rocks.

Nephelinite is an example of a silica-undersaturated igneous rock. The degree of silica saturation can be evaluated with

polymorph). Silica-undersaturated mafic igneous rocks contain magnesian olivine but not magnesian orthopyroxene, and/or a feldspathoid
. Silica-saturated igneous rocks fall in between these two classes.

Silica-undersaturated, mafic igneous rocks are much less abundant than silica-saturated and oversaturated basalts. Genesis of the less common mafic rocks such as nephelinite is usually ascribed to more than one of the following three causes:

  • relatively high pressure of melting;
  • relatively low degree of fractional melting in a mantle source;
  • relatively high dissolved carbon dioxide in the melt.

Nephelinites and similar rocks typically contain relatively high concentrations of elements such as the light rare earths, as consistent with a low degree of melting of mantle peridotite at depths sufficient to stabilize garnet. Nephelinites are also associated with carbonatite in some occurrences, consistent with source rocks relatively rich in carbon dioxide.

Nephelinite is found on ocean islands such as

Nyiragongo, another African volcano known for its semipermanent lava lake activity, erupts lava made of melilite nephelinite. The unusual chemical makeup of this igneous rock
may be a factor in the unusual fluidity of its lavas.

Columnar jointing in melilite-olivine nephelinite from the Southern Balcones volcanic and intrusive rocks, Uvalde County, Texas.

Olivine nephelinite flows also occur in the

Yukon Territory. Melilite olivine nephelinite intrusives of Cretaceous age are found in the area around Uvalde, Texas
.

References

Bibliography

Flett, John Smith (1911). "Nephelinites" . In Chisholm, Hugh (ed.). Encyclopædia Britannica
. Vol. 19 (11th ed.). Cambridge University Press. p. 384.

External links