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Epidote group

Dissakisite-(Ce) is a new member of the epidote group from Antarctica and a Mg-analogue of allanite-(Ce) (Grew et al. 1991). The number of octahedral Mg sites, one. [Pg.429]

Nesosilicates is the class of silicate minerals in which the structure is built up by independent tetrahedra of SiOa. This class contains some mineral groups like the olivines, the silicate garnets, the epidote group and some separate minerals. [Pg.130]

W.A. Dollase, Mossbauer spectra and iron distribution in the epidote-group minerals. Z. Krist. 138, 41-63 (1973)... [Pg.178]

Sorosilicates consist of two joined silica tetrahedra, which are otherwise isolated, and the epidote group minerals are the most common variety of this case. [Pg.341]

See other pages where Epidote group is mentioned: [Pg.203]    [Pg.74]    [Pg.104]    [Pg.109]    [Pg.174]    [Pg.291]    [Pg.336]    [Pg.22]    [Pg.427]    [Pg.428]    [Pg.428]    [Pg.429]    [Pg.802]    [Pg.818]    [Pg.823]    [Pg.848]    [Pg.867]    [Pg.163]    [Pg.133]    [Pg.23]    [Pg.23]    [Pg.7]   


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Epidote

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