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- W4315694713 abstract "In this chapter we discuss the role of groundwater in compaction and diagenesis. Compaction refers to the mechanical reduction in porosity that occurs in sedimentary sequences as they undergo depositional or tectonic loading and increases in effective stress. Diagenesis of sedimentary sequences refers to all of the chemical, physical, and biological changes undergone by a sediment after its initial deposition and during and after lithification, exclusive of weathering and metamorphism (Jackson, 1997). By this broad definition, diagenesis actually encompasses mechanical compaction, a process that we distinguish here for purposes of discussion: we discuss mechanical compaction in Section 11.1 and other forms of diagenesis in Section 11.2." @default.
- W4315694713 created "2023-01-12" @default.
- W4315694713 date "2006-05-04" @default.
- W4315694713 modified "2023-09-23" @default.
- W4315694713 title "Compaction and diagenesis" @default.
- W4315694713 doi "https://doi.org/10.1017/9780511807855.012" @default.
- W4315694713 hasPublicationYear "2006" @default.
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