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Gehlenite, (Ca2Al[AlSiO7]), is a sorosilicate, Al-rich endmember of the melilite complete solid solution series with akermanite. The type locality is in the Monzoni Mountains, Fassa Valley in Trento Province in Italy, and is named after Adolf Ferdinand Gehlen by A.J. Fuchs in 1815.
Additional recommended knowledge
Gehlenite is found in carbonaceous chondrites from which it condensed as a refractory mineral in the hotter stages (FU Ori) of the presolar nebula , and is found in diorite intruded carbonate rocks , and to a far lesser extent in uncompahgrites , melilitites , alnoites , lamprophyres and possibly kimberlite pipes.
Gehlenite has also been found on the comet 81P/Wild.
Crystallography, Composition and Physical Properties
Gehlenite is one of five, isostructural tetragonal crystal system minerals in the melilite group. The tetrahedral linkage within the structure is similar to that of an aluminosilicate framework structure and was once considered a feldspathoid-like mineral due to silica undersaturation.
Gehlenite has a Mohs hardness of 5-6, a vitreous to greasy lustre, distinct to good cleavage and is yellow brown, greenish grey or colourless. Its streak is white or grey-white.  It is uniaxial (-), has an anomolous nonzero 2V angle and has a characteristic 'ultrablue' birefringence.
|This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Gehlenite". A list of authors is available in Wikipedia.|