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Chlorite macroscopic

Hydrothermal studies by Roy and Romo (1957) indicate that macroscopic vermiculite cannot form above 200-300°C. At these temperatures some of the octahedral ions migrate into the interlayer positions and a chlorite-like phase is formed. [Pg.106]

See other pages where Chlorite macroscopic is mentioned: [Pg.87]    [Pg.87]    [Pg.99]    [Pg.100]    [Pg.302]    [Pg.11]    [Pg.220]    [Pg.156]    [Pg.157]   
See also in sourсe #XX -- [ Pg.87 , Pg.88 , Pg.89 , Pg.90 ]



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Chlorite

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