Here is a comprehensive and up to-do-date presentation of the
origins, and properties of clay minerals at the Earth?'s surface.
The text reviews the relatively simple laws that govern the
chemical or isotopic composition and the crystalline structure of
clays, and then discusses their genesis and alteration. Concluding
chapters show that clay minerals can form in variety of different
environments: meteorites, lavas, subduction zones, among
others.
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