Abstract
Generally when one considers alteration sequences one thinks of climates and conditions common to one’s environment; i.e. inhabited, agricultural areas. However some climatic conditions create special chemical systems where specific minerals form due to the climate, i.e. variations of total rainfall and rainfall distribution throughout a yearly cycle. Of course one can consider glacial conditions as a climate. But given that very little of the yearly interaction with rock and atmosphere occurs under conditions of liquid water/rock interaction, this climatic possibility is ignored here. Very cold, tundra, climates tend to be more assimilable to those of temperate climate systems but these systems operate only part of the year and biological activity is weak.
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Suggested Reading
Fitzpatrick E (1983) Soils. Longman, London, 353 pp
Jenny H (1994) Factors of soil formation. Dover, New York, 281 pp
Millot G (1964) Géologie des argiles. Masson and Cie, Paris, 499 pp (English translation 1970: Geology of clays. Springer-Verlag, New York, 429 pp)
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© 2008 Springer-Verlag Berlin Heidelberg
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Velde, B., Meunier, A. (2008). Clays and Climate – Clay Assemblages Formed under Extreme Humidity Conditions. In: The Origin of Clay Minerals in Soils and Weathered Rocks. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-75634-7_6
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DOI: https://doi.org/10.1007/978-3-540-75634-7_6
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-540-75633-0
Online ISBN: 978-3-540-75634-7
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