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Silicates, general structural rules

General rules governing the structures of natural silicates... [Pg.543]

The structures of natural silicates obey the following general rules ... [Pg.543]

Veitch and Radoslovich [1963] postulate that there should be two distinct octahedral hole sizes for most layer silicates and that octahedral ordering should exist as a general rule. This is only partly true for the chlorites whose structures are known. The llb-2 prochlorite shows cation ordering within both octahedral sheets. The la-4 kammererite and llb-4 corundophilite structures are ordered within the interlayer only. [Pg.236]

See other pages where Silicates, general structural rules is mentioned: [Pg.302]    [Pg.108]    [Pg.111]    [Pg.62]    [Pg.61]    [Pg.288]    [Pg.215]    [Pg.240]    [Pg.241]    [Pg.275]    [Pg.243]    [Pg.253]    [Pg.422]    [Pg.231]    [Pg.760]    [Pg.348]    [Pg.1021]    [Pg.95]    [Pg.671]    [Pg.411]    [Pg.78]   
See also in sourсe #XX -- [ Pg.543 ]



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