Jump to content

Leucophanite

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by InternetArchiveBot (talk | contribs) at 23:50, 21 December 2017 (Rescuing 1 sources and tagging 0 as dead. #IABot (v1.6.1)). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Leucophanite
The leucophanite on an aegirine needle (about 4-5 mm on edge)
General
CategoryInosilicates
Formula
(repeating unit)
(Na,Ca)2BeSi2(O.OH.F)7
Strunz classification9.DH.05
Crystal systemOrthorhombic
Crystal classDisphenoidal (222)
(same H-M symbol)
Space groupP212121
Identification
References[1][2][3][4][5]

Leucophanite is an inosilicate mineral with a complex composition, (Na,Ca)2BeSi2(O.OH.F)7. It may contain cerium substituting in the calcium position.

It occurs in pegmatites and alkali igneous complexes as yellow, greenish or white triclinic crystals and has been found in Norway, Quebec and Russia.

It was first described from the Langesundfiord district of southern Norway in 1840. The name is from the Greek leucos for "white" and phanein for "to appear" in allusion to the common white color.

References