Time dependence of the rate and direction of mineral weathering and clay mineral formation with special consideration to kaolinites

  This paper summarizes mineralogical results from temperate, subtropical and tropical soil chrono- and climosequences and aims to understand the role of the factor time for the formation of kaolinites. A mid-Pleistocene welded F6-paleosol at Stari Slankamen, Serbia, developed discontinuously in a...

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Bibliographic Details
Main Author: Arnt Bronger
Format: Article
Language:English
Published: Universidad Nacional Autónoma de México 2018-01-01
Series:Revista Mexicana de Ciencias Geológicas
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Online Access:https://rmcg.unam.mx/index.php/rmcg/article/view/710
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