Definition
Diagenesis is the sum total of processes that occur following deposition of a sediment up to but excluding metamorphism. It includes compaction, mineral precipitation, mineral dissolution, and mineral transformation. Many of the processes contribute to lithification , the conversion of sediment into rock.
Introduction
The word “diagenesis” (Greek dia meaning “passing through” and Latin genesis, “development or generation”) was first used in geology in 1868 by the German geologist Wilhelm von Gümbel. The term was refined by Johannes Walther in his work “Introduction to Geology as a Historical Science” (Einleitung in die Geologie als historische Wissenschaft, 1893–1894) and by William T. Twenhofel in Principles of Sedimentation (1939) to its current definition.
Diagenesis is key to understanding the evolution of rock composition and texture with depth, time, and temperature and to deciphering the mechanisms by which elements are cycled between the atmosphere, ocean, and crust....
References
Aplin AC, McQuaker JHS (2011) Mudstone diversity: origin and implications for source seal and reservoir properties in petroleum systems. AAPG Bull 95:2031–2059
Baldwin B, Butler CO (1985) Compaction curves. AAPG Bull 69:622–626
Bjørlykke K (2015) Petroleum geoscience: from sedimentary environments to rock physics, 2nd edn. Springer, Heidelberg, 662 p
Blenkinsop TG (1998) Definition of low-grade metamorphic zones using illite crystallinity. J Metamorph Geol 6:623–636
Burley SD, Worden R (2003) Sandstone diagenesis: recent and ancient. Reprint series volume 4 of the International Association of Sedimentologists. Wiley, New York, 656 p
Clark SJ (2014) Constraining diagenetic timings, processes and reservoir quality in igneous-affected basins. PhD dissertation, Durham University
Davies RJ, Cartwright J (2002) A fossilized opal A to opal C/T transformation on the northeast Atlantic margin: support for a significantly elevated paleogeothermal gradient during the Neogene? Basin Res 14:467–486
Emery D, Robinson AG (1993) Inorganic geochemistry: applications to petroleum geology. Blackwell Scientific Publications, Oxford, 255 p
Gluyas JG, Cade CA (1997) Prediction of porosity in compacted sands. In: Kupecz J, Gluyas JG, Bloch S (eds) Reservoir quality prediction in sandstones and carbonates. American Association of Petroleum Geologists Memoir, vol 69. pp 19–28
Gluyas JG, Leonard AJ (1995) Diagenesis of the Rotliegend sandstone: the answer ain’t blowin’ in the wind. Mar Pet Geol 12:491–497
Gluyas JG, Swarbrick RE (2004) Petroleum geoscience. Blackwell, Oxford, 359 p
Goldhammer RK (1997) Compaction and decompaction algorithms for sedimentary carbonates. J Sedimen Res A 67:26–35
Halley RB, Schmoker JW (1983) High-porosity Cenozoic carbonate rocks of South Florida: progressive loss of porosity with depth. AAPG Bull 67:191–200
Irwin H, Curtis CD, Coleman ML (1977) Isotopic evidence for source of diagenetic carbonates formed during burial of organic-rich sediments. Nature 269:209–213
Milliken KL, Rudnicki M, Awwiller DN, Zhang T (2012) Organic matter-hosted pore system, Marcellus formation (Devonian), Pennsylvania. AAPG Bull 97:177–200
Oertel G, Curtis CD (1972) Clay-ironstone concretion preserving fabrics due to progressive compaction. Geol Soc Am Bull 83:2597–2606
Oxtoby NH, Mitchell AW, Gluyas JG (1995) The filling and emptying of the Ula oilfield: fluid inclusion constraints. In Cubitt JM, England WA (eds) The geochemistry of reservoirs. Geological Society, London, Special Publications, vol 86. Geological Society, London, pp 141–157
Primmer TJ, Cade CA, Evans IJ, Gluyas JG, Hopkins MS, Oxtoby NH, Smalley PC, Warren EA, Worden RH (1997) Global patterns in regional diagenesis – their application to reservoir quality prediction for petroleum exploration. In: Kupecz JA, Gluyas J, Bloch S (eds) Reservoir quality prediction in sandstones and carbonates. AAPG memoir, vol 69. pp 61–78
Read, JF, Horbury AD (1993) Eustacy and tectonic controls on porosity evolution beneath sequence-bounding unconformities and paeasequence disconformities on carbonate platforms. In: Horbury AD, Robinson AG (eds) Diagenesis and basin development. American Association of Petroleum Geologists studies in geology, vol 36. pp 155–198
Robinson AG, Coleman ML, Gluyas JG (1993) The age and cause of illite cement growth, village fields area, southern North Sea: evidence from K-Ar ages and 18O/16O ages. AAPG Bull 77:68–80
Vesic AS, Clough GW (1968) Behaviour of granular material under high stresses. J Soil Mech Found Div 94:661–688
Walls JD, Diaz E, Derzhi N, Grader A, Dvorkin J, Arredondo S, Caprio G (2011) Eagle ford shale reservoir properties from digital rock physics, 2011 CSPG CSEG CWLS convention, http://www.cspg.org/cspg/documents/Conventions/Archives/Annual/2011/048-Eagle_Ford_Shale_Reservoir_Properties.pdf. Accessed on 21 Aug 2017
Yuan G, Cao Y, Gluyas JG, Li X, Xi K, Wang Y, Jia Z, Sun P, Oxtoby NH (2015) Feldspar dissolution, authigenic clays and quartz cement in open and closed geochemical systems during diagenesis: typical examples from two rift sags in Bohai Bay, East China. AAPG Bull 99:2121–2154
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Gluyas, J.G., Yuan, G. (2018). Diagenesis. In: Sorkhabi, R. (eds) Encyclopedia of Petroleum Geoscience. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-02330-4_123-1
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DOI: https://doi.org/10.1007/978-3-319-02330-4_123-1
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