| 1. | The aluminium hydroxide in the lateritic bauxite deposits is almost exclusively gibbsite.
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| 2. | Gibbsite and bayerite are monoclinic, whereas doyleite and nordstrandite are triclinic forms.
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| 3. | As well as the process of catalyst substrates from gibbsite were also investigated.
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| 4. | Minerals formed in laterite nickel deposits include gibbsite.
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| 5. | Now, the main question is about gibbsite formation in the middle of kaolin series.
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| 6. | The basic structure of corundum is identical to gibbsite except the hydroxides are replaced by oxygen.
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| 7. | Gibbsite's structure is closely related to the structure of brucite, Mg ( OH ) 2.
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| 8. | The different symmetry of gibbsite and brucite is due to the different way that the layers are stacked.
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| 9. | It occurs in association with basaluminite, gibbsite, epsomite, gypsum, celestine, dolomite and goethite.
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| 10. | We thus should find the hyper-aluminous materials, containing gibbsite in the lower series of kaolin.
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