Essexite

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Craigleith, an island in Scotland, composed of essexite

Essexite (

plutonic igneous rock. Its name is derived from the type locality in Essex County, Massachusetts, in the United States
.

Modern

IUGS QAPF diagram of Streckeisen (1974) "essexite" is more formally known as nepheline monzodiorite or nepheline monzogabbro depending on the ratio of orthoclase to plagioclase and the abundance of nepheline.[3]

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

alkaline igneous rock equivalent to an alkaline basalt. The presence of nepheline, a feldspathoid mineral, indicates that essexites are silica undersaturated. The presence of orthoclase indicates that it contains sufficient potassium to favor production of orthoclase over microcline or potassic oligoclase
.

Essexites are generally rich in aluminium, alkalis (sodium and calcium), potassium (>3% K2O), LILE-enriched (

tholeiitic basalts
and gabbros.

References

  1. ^ "nepheline". Dictionary.com Unabridged (Online). n.d. Retrieved 2016-01-23.
  2. ^ "nepheline". Merriam-Webster.com Dictionary. Retrieved 2016-01-23.
  3. ^ 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