Abstract
Like desert, glacier and river deposits, lake sediments may include most of the minerals issued from igneous, metamorphic and sedimentary rocks. This is especially the case of freshwater sediments, that commonly include numerous nonclay and clay silicates, various carbonates, Fe-Mn oxides, phosphates, sulfides, and fluorides (see Jones and Bowser’s review, 1978). Mite and smectite constitute the dominant species, and are as frequently encountered as quartz. Chlorite, kaolinite, mixed-layers and palygorskite are variously present, depending on the lake location. A general correspondence exists between the mineral composition of most freshwater lakes and the average clay mineralogy of rocks and soils in the surrounding drainage basins. Let us consider a few selected examples.
Keywords
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
This is a preview of subscription content, log in via an institution.
Buying options
Tax calculation will be finalised at checkout
Purchases are for personal use only
Learn about institutional subscriptionsPreview
Unable to display preview. Download preview PDF.
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 1989 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
Chamley, H. (1989). Lacustrine Clay Sedimentation. In: Clay Sedimentology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-85916-8_4
Download citation
DOI: https://doi.org/10.1007/978-3-642-85916-8_4
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-85918-2
Online ISBN: 978-3-642-85916-8
eBook Packages: Springer Book Archive