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Kaolinite geochemistry

De Putter, T., Andre, L., Bernard, A., Dupuis, C., Jedwab, J., Nicaise, D. Perruchot, A. 2002. Trace element (Th, U, Pb, REE) behaviour in a cryptokarstic halloysite and kaolinite deposit from Southern Belgium importance of accessory mineral formation for radioactive pollutant trapping. Applied Geochemistry, 17, 1313-1328. [Pg.119]

McLaughlin, R.J.W., 1959. The geochemistry of some kaolinitic clays. Geochim. Cosmochim. Acta, 17 11-16. [Pg.198]

Tardy, Y., and D. Nahon. 1985. Geochemistry of laterites, stability of Al-goethite, Al-hematite, and Fe -kaolinite in bauxites and ferricretes An approach to the mechanism of concretion formation. Am. J. Sci. 285 865-903,... [Pg.586]

Alcantara T, Pazos M, Cameselle C, Sanromdn MA. (2008a). Electrochemical remediation of phenanthrene from contaminated kaolinite. Environmental Geochemistry and Health... [Pg.465]

The material source of the watershed fault zone is both from host rock and overlying siliceous rocks. The fault zone is an open system with strong chemical weathering, and alkaline condition. Calcium in limestone is leached, the cohesive force of host rock is reduced and formed smectite. It is easy for feldspar transforms to kaolinite under alkaline condition during faulting. Hence, more geochemistry needed to study in the future, to establish qualitative model between chemical compositions and strength of fault rocks. [Pg.84]

See other pages where Kaolinite geochemistry is mentioned: [Pg.251]    [Pg.634]    [Pg.180]    [Pg.868]    [Pg.2307]    [Pg.868]    [Pg.188]    [Pg.300]    [Pg.306]    [Pg.81]    [Pg.235]   
See also in sourсe #XX -- [ Pg.868 ]

See also in sourсe #XX -- [ Pg.868 ]

See also in sourсe #XX -- [ Pg.6 , Pg.868 ]



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