By Stuart Burley, Richard Worden
Diagenesis impacts all sediments after their deposition and encompasses a basic suite of actual, chemical and organic techniques that keep an eye on the feel, mineralogy and fluid-flow homes of sedimentary rocks. figuring out the approaches and items of diagenesis is hence a severe part within the research of the evolution of sedimentary basins, and has functional implications for subsurface porosity destruction, protection and new release. This in flip is of significant relevance to the petroleum and water industries, in addition to to the positioning and nature of a few fiscal mineral deposits.
- Combines key papers in sandstone diagenesis released in Sedimentology during the last 30 years.
- Records the improvement of diagenesis from the outline of grain shapes via provenance, petrography and analytical geochemistry to predictive versions of diagenetic procedure.
- Provides definitions and factors of the phrases and ideas utilized in diagenesis.
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Additional resources for Sandstone Diagenesis: Recent and Ancient (Reprint Series 4 of the IAS) (International Association Of Sedimentologists Reprints)
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American Association of Petroleum Geologists Bulletin, 75, 1547-1562. Esteoule-Choux, J. (1983) Kaolinitic weathering profiles in Brittany: genesis and economic importance. In: Residual Deposits: Surface Related Weathering Processes and Materials (Ed. L. Wilson). Spec. Publ. Geol. Soc. London, No. 11, pp. 33-38. Blackwell Scientific Publications, Oxford. L. (1965) Some aspects of recrystallisation in ancient limestones. C. G. Murray). Spec. Publ. Soc. Econ. Paleont. , Tulsa, OK, 13, 14-48. Frey, M.
Electron) microscope is known as microporosity. Porosity that is visible with the naked eye is termed macroporosity. 33 Porosity that occurs between primary sand grains and that was present at deposition of the sediment is known as primary porosity. Porosity that develops during diagenetic processes such as mineral dissolution is termed secondary porosity. Porosity that develops at a site formerly occupied by a mineral that dissolved and reprecipitated locally elsewhere in the rock is known as redistributional secondary porosity (as no new porosity is created).
1989). The characteristic feature of largescale fluid migration is the potential for mixing zones to occur that are preferentially the loci of intense diagenetic reaction (Giles, 1987). Widespread flow of aqueous fluids from mudstones 27 has been thought to be responsible for the growth of (locally zoned) ankerite in sandstones (Gawthorpe, 1987; Mozley & Joernle, 1990). Basin-scale water flow can take place at any stage during the evolution of a sedimentary basin (Fig. 18). In the early stages of basin formation large-scale water flow is usually driven by topographic head (Bethke & Marshack, 1990).