Reservoirs generally consist of sandstones or carbonates exhibiting heterogeneities caused by a wide range of factors. Some of these formed depositionally (e.g. as channels, palaeosols, clay seams or salts), others may be diagenetic in origin (e.g. carbonate or silica cemented zones, authigenic clays, karstic surfaces). The severity with which diagenesis affects rock systems results from the interplay between the diagenetic process itself and the timescale over which it operated. The book provides a wide-ranging overview of diagenetic processes and responses in calcareous, argillaceous, arenaceous and carbon-rich (microbial and organic) sedimentary systems. It introduces diagenetic concepts, reviews existing knowledge, and shows how existing qualitative approaches might be developed in more quantitative ways. Several chapters consider mass balance calculations and the temporal and spatial aspects of diagenetic processes. It is unique, as a textbook, in providing such a breadth of diagenetic subject range and such depth of coverage in each topic. It provides a source reference for advanced students and professionals active in reservoir and aquifer studies.

Product Description: Offers a comprehensive discussion of the geochemistry of sedimentary sulfur, including low temperature transformation in early diagenesis, thermal reactions occurring during later diagenesis and catagenesis. Provides a detailed examination of sulfur-organic matter interactions...read more

Product Description: Process quantification has wrought major changes in the field of sedimentary geochemistry, often resulting in more rigorous descriptions that challenge conventional wisdom. This edited volume presents a survey of those changes, from controls on sediment input to its deep burial in sedimentary basins...read more