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- W4242692530 abstract "Publisher SummaryThis chapter discusses the compaction of argillaceous sediments. The genesis of clay minerals is associated with the compaction, burial, and diagenesis of argillaceous sediments. Clay minerals that comprise argillaceous sediments owe their origin to three principal processes: (1) detrital inheritance from preexisting rocks and sediments; (2) transformation of the clays from one form to another in the sedimentary environment owing to their instability at low temperatures and various ranges of pH and Eh; and (3) neoformation of clay minerals in situ. The most important allogenic components of argillaceous sediments include various clay minerals, including gibbsite, quartz, feldspars, carbonates, amorphous silica and alumina, pyroclastic material, and organic matter. The initial water content of most argillaceous muds is approximately 50-80%, which corresponds to a porosity of 70-90%. In sands, on the other hand, porosity is only 30-50%, which corresponds to 20-30% water content. The chapter also discusses some fundamental fluid mechanics concepts, mechanics of compaction, and diagenesis–metamorphism transition phase." @default.
- W4242692530 created "2022-05-12" @default.
- W4242692530 date "1974-01-01" @default.
- W4242692530 modified "2023-10-16" @default.
- W4242692530 title "Chapter 1 Introduction" @default.
- W4242692530 doi "https://doi.org/10.1016/s0070-4571(08)70771-4" @default.
- W4242692530 hasPublicationYear "1974" @default.
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