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UNIVERSIDAD COMPLUTENSE DE MADRID

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carbon deposition on transition metal- and uranium-oxides

THE CRYSTAL CHEMISTRY OF KORNERUPINE
where r is the gyromagnetic ratio, H 0 is the external magnetic field, H D is the Dzyaloshinsky field, H A is the magnetic anisotropy field. Using (10) we 
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0¿ -S iO z graphi te*methane. Fe 2Si04-FeSi0s-Fe Fe2*, Mg. C = Mg, Fe2*, Mn, ?1, Fe3*, Ti, Li. T ratio of about 0.88 for cations assigned to the.
Microscopic Determination of . the Nonopaque Minerals
Fe3* as compared to columbite-tantalite. Structural analysis of a partially disordered tapio- lite shor¡ed it to be 74% otdered with â trirutile structure 
AN 1ao/160 STUDY OF MESOZOIC AND EARLY TERTIARY
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Fe2 and Fe3 sites top view, d) Fe2 and Fe3 sites side .9S1.1 to FeAs1.1S0.9. [36]. It is a diamagnetic 0 to 1. Values close to 1 mean that, in the.