
Gmelinite is a series of rare zeolite minerals. The most common member is gmelinite-Na; others are gmelinite-Ca and gmelinite-K. It is closely related to the very similar mineral chabazite. Gmelinite was named as a single species in 1825 after Christian Gottlob Gmelin (1792–1860) professor of chemistry and mineralogist from Tübingen, Germany, and in 1997 it was raised to the status of a series.Gmelinite-Na has been synthesised from Na-bearing aluminosilicate gels. The naturally occurring mineral forms striking crystals, shallow, six sided double pyramids, which can be colorless, white, pale ye
via Wikipedia infobox
{{Infobox mineral | name = Gmelinite | category = Tectosilicate minerals | group = Zeolite group | image = Gmelinite-Na-Chabazite-Ca-153544.jpg | imagesize = 260px | caption = | formula = | IMAsymbol = Gmelinite-Na: Gme-Na | molweight = 2,000.77 g | strunz = 9.GD.05 (10 ed) 8/J.26-50 (8 ed) | dana = 77.1.2.6 | system = Hexagonal | class = Dihexagonal dipyramidal (6mmm) H-M symbol: (6/m 2/m 2/m) | symmetry = P63/mmc | unit cell = a = 13.78, c = 10.03 [Å]; Z = 4 | color = Colorless, white, yellow, orange, pale green, pink, red, brown and grey | habit = Hexagonal plates, or short prisms, showing hexagonal dipyramids, pyramids and basal pinacoid. {100}, {101} and {0001} dominant. May also be tabular or rhombohedral. Crystals are striated parallel to (0001) | twinning = Interpenetrant twins common on {101}. The twins consist of four individuals, three are at 90° to the other and at 60° to each other | cleavage = Good on {100} | fracture = Conchoidal | tenacity = Brittle | mohs = | luster = Dull to vitreous | refractive = nω = 1.476 - 1.494, nε = 1.474 - 1.480 | opticalprop = Uniaxial (-) | birefringence = δ = 0.002 - 0.014 | pleochroism = | streak = White | gravity = 2.04 to 2.17 | density = | melt = | fusibility = | diagnostic = | solubility = Soluble in cold 10% HCl. | diaphaneity = Transparent, translucent or opaque | other = Piezoelectric. Barely detectable radioactivity. As with all zeolites, water is released on heating, and almost all has been expelled by 400 °C. | references = }}
Gmelinite is a series of rare zeolite minerals. The most common member is gmelinite-Na; others are gmelinite-Ca and gmelinite-K. It is closely related to the very similar mineral chabazite. Gmelinite was named as a single species in 1825 after Christian Gottlob Gmelin (1792–1860) professor of chemistry and mineralogist from Tübingen, Germany, and in 1997 it was raised to the status of a series.Gmelinite-Na has been synthesised from Na-bearing aluminosilicate gels. The naturally occurring mineral forms striking crystals, shallow, six sided double pyramids, which can be colorless, white, pale yellow, greenish, orange, pink, and red. They have been compared to an angular flying saucer.
Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).