Essexite
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Essexite (
Modern
Petrology
In order to produce a
The source melts of essexites contain more aluminium and alkali ions than available silica tetrahedra, which is why essexites crystallise nepheline instead of plagioclase. Higher than normal potassium favors the production of orthoclase, which is usually absent from most mafic igneous rocks.
Mineralogy
Essexite can be considered as an alkali gabbro or monzodiorite primarily composed of nepheline, plagioclase, with lesser amounts of alkali feldspar, with mafic minerals composed of any of the following; titanium augite (pyroxene), hornblende and biotite.
Trace mineralogy may include magnetite, ilmenite and accessory olivine (<5%).
Essexite grades into a nepheline monzogabbro with a decrease in potassium feldspar and an increase in the feldspathoid minerals.
Geochemistry
Essexite is an
Essexites are generally rich in aluminium, alkalis (sodium and calcium), potassium (>3% K2O), LILE-enriched (
References
- ^ "nepheline". Dictionary.com Unabridged (Online). n.d. Retrieved 2016-01-23.
- ^ "nepheline". Merriam-Webster.com Dictionary. Retrieved 2016-01-23.
- ^ Henry, Darrell. "Classification of Igneous Rocks - Flow Chart". Geology 3041: Igneous and Metamorphic Petrology Lectures. Louisiana State University. Archived from the original on 10 May 2008. Retrieved 1 March 2006.
External links
- Russian alkaline igneous rock occurrences Archived 2008-08-28 at the Wayback Machine