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Olivine covalent bonding

Finally, other factors, including the increased covalent bonding with bridging oxygen atoms in the amphibole M4 and pyroxene M2 sites and the slightly larger ionic character of the olivine Ml site, also influence distributions of the cations in coexisting minerals. [Pg.291]

See other pages where Olivine covalent bonding is mentioned: [Pg.168]    [Pg.268]    [Pg.434]    [Pg.3624]    [Pg.241]    [Pg.253]    [Pg.3623]    [Pg.69]    [Pg.270]    [Pg.362]    [Pg.73]    [Pg.322]    [Pg.418]    [Pg.95]    [Pg.446]    [Pg.60]    [Pg.54]    [Pg.493]    [Pg.495]    [Pg.250]    [Pg.550]   
See also in sourсe #XX -- [ Pg.268 ]



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Olivine

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