Abstract
Freshly deposited sediments are commonly unconsolidated, have a relatively low bulk density and high permeability and, if accumulated under water, a high water content. However, with increasing burial depth under younger sediments, and occasionally shortly after deposition, the sediments become denser and more solid or lithified. All the processes involved in such a change of sediment state are summarized under the term diagenesis. It comprises both mechanical and chemical-mineralogical processes.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 1992 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
Einsele, G. (1992). Mechanical and Chemical Diagenesis. In: Sedimentary Basins. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-77055-5_13
Download citation
DOI: https://doi.org/10.1007/978-3-642-77055-5_13
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-540-54449-4
Online ISBN: 978-3-642-77055-5
eBook Packages: Springer Book Archive