Talk:Silicate mineral

Latest comment: 1 year ago by Smokefoot in topic Not a merge proposal, but issues still

..."discussed in chapter 15"? Was this paragraph lifted from a textbook? Anyway, it's not linked well to the text. — Preceding unsigned comment added by 83.203.108.46 (talk) 01:43, 26 March 2018 (UTC)Reply

Diagrams?

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Just a friendly suggestion to the editors. It's not entirely clear what these structures look like from the written descriptions. Diagrams would be helpful. MAzari 03:28, 30 October 2006 (UTC)Reply

Analcime

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Analcime appears twice. As part of the Feldspathoid group and as a stand alone mineral in the Tectosilicates subclass. Which one should be deleted? Avihu (talk) 10:32, 20 April 2008 (UTC)Reply

Removed from the feldspathoid group. The classification was originally set up following the Hurlbut and Klein reference which lists analcime separately. I note that the online refs include it in the zeolite group as the analcime article says (with qualification). Vsmith (talk) 14:08, 20 April 2008 (UTC)Reply

Albite

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Albite appears twice: First, as part of the alkali-feldspars; second, as part of the plagioclase feldspars. Which one should be deleted? (My imperfect memory is, albite belongs to the second group, but not the first.) Someone please check and fix. The feldspars are really common, and it's really important for Wikipedia to get this right. Oaklandguy (talk) 17:37, 28 August 2013 (UTC)Reply

Discrete SiO4 4- ions in neso silicates

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Aren't neso silicates such as phenakite better described as containing close packed oxide ions with silicon in tetrahedral positions, rather than as containing discrete SiO44- ions with interstitial cations? Surely these are mixed oxides. Axiosaurus (talk) 09:38, 8 February 2013 (UTC)Reply

It doesn't make a difference as it is a continous crystalline network with a repeating unit. --Chris.urs-o (talk) 03:39, 10 February 2013 (UTC)Reply
Yes obviously, neso-silicates are after all crystalline! Saying there are discrete SiO44- ions with interstitial cations, is very different from saying there are Si atoms in tetrahedral positions in a close packed structure. Axiosaurus (talk) 16:38, 11 February 2013 (UTC)Reply
Rruff (IMA) says the repeating unit is Be2SiO4, CNMNC's (IMA) master list (2012 version) says the same. --Chris.urs-o (talk) 15:22, 13 February 2013 (UTC)Reply

"Sorosilicate"

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Sōros is indeed Greek for 'heap', but what does this mineral group have to do with that? Given the "twinned" SiO₄ tetrahedra, I would suspect that whoever named this rather slipped into Latin, where soror is 'sister'. Anyone willing to dig into a source or two on this? --Trɔpʏliʊmblah 02:54, 27 February 2017 (UTC)Reply

Cyclosilicates

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Under Main groups:

   Nesosilicates (isolated silicon tetrahedra) – [SiO4]4−, e.g. olivine.
   Sorosilicates (double tetrahedra) – [Si2O7]6−, e.g. epidote, melilite group.
   Cyclosilicates (rings) – [SinO3n]2n−, e.g. tourmaline group.
   Inosilicates (single chain) – [SinO3n]2n−, e.g. pyroxene group.
   Inosilicates (double chain) – [Si4nO11n]6n−, e.g. amphibole group.
   Phyllosilicates (sheets) – [Si2nO5n]2n−, e.g. micas and clays.
   Tectosilicates (3D framework) – [AlxSiyO2x+2y)]x−, e.g. quartz, feldspars, zeolites.

Some categories use n, other x,y In the details below, for instance" Cyclosilicates (from Greek κύκλος kuklos, circle), or ring silicates, have three or more tetrahedra linked in a ring. The general formula is (SixO3x)2x− Cyclosilicates under details uses x, under Main group uses n. Which is proper?Dweisman (talk) 06:13, 14 October 2018 (UTC)Reply

Not a merge proposal, but issues still

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It is no crisis, but silicate and silicate mineral have a lot of overlap. --Smokefoot (talk) 15:53, 28 November 2022 (UTC)Reply