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Olivine iron/magnesium ratios

Bartholome, P., 1962. Iron-magnesium ratio in associated pyroxenes and olivines. Geol. Soc. Am., Petrologic Studies A volume in honour of A.F. Buddington, New York, pp. 1-20. [Pg.283]

Different soils contain different mineral structures and thus exhibit varying properties. Olivines contain elements including iron and magnesium. Other species, such as quartz, contain only silicon and oxygen, whereas feldspar is a mineral containing a fixed 1 4 ratio of aluminum to silicon. Clays, such as kaolinite, are more complex structures that contain layers of minerals arranged in sheets, often with... [Pg.53]

See other pages where Olivine iron/magnesium ratios is mentioned: [Pg.356]    [Pg.1236]    [Pg.106]    [Pg.1152]    [Pg.354]    [Pg.177]    [Pg.35]    [Pg.415]    [Pg.748]    [Pg.826]    [Pg.124]    [Pg.489]    [Pg.19]    [Pg.519]    [Pg.410]    [Pg.79]   


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