Sedimentology

2003 Edition
| Editors: Gerard V. Middleton, Michael J. Church, Mario Coniglio, Lawrence A. Hardie, Frederick J. Longstaffe

Authigenesis

  • James R. Boles
Reference work entry
DOI: https://doi.org/10.1007/978-1-4020-3609-5_13

Overview

Authigenesis refers to processes by which minerals form, in place, within sediments and sedimentary rocks. Such minerals are referred to as authigenic minerals. In contrast, detrital minerals are erosion products deposited in the depositional environment. Diagenesis refers to the physical and chemical changes that occur in sediments after they are deposited (or precipitated). All authigenic minerals form within this context. The formation of authigenic minerals is a result of the presence of unstable mineral grains, biological modification of the sediment, grain deformation and fracturing, flux of various fluids through the sediment, and changing burial conditions. The intrinsic value of most sediments is their ability to hold fluid such as water and hydrocarbons. From an economic viewpoint, authigenesis is important because it influences the porosity (void volume in the rock) and permeability of the rock (ability of the rock to transmit fluid).

Authigenic minerals can reveal...

This is a preview of subscription content, log in to check access.

Bibliography

  1. Bjorlykke, K., and Aagaard, P., 1992. Clay minerals in North Sea sandstones In Origin, Diagenesis and Petrophysics of Clay Minerals in Sandstones, SEPM, Special Publication, 37, 65–80.Google Scholar
  2. Boles, J.R., 1982. Active albitization of plagioclase, Gulf Coast Tertiary. American Journal of Science, 282: 165–180.Google Scholar
  3. Boles, J.R., 1998. Carbonate cementation in Tertiary sandstones of the San Joaquin Basin. In Morad, S. (ed.), Carbonate Cementation in Sandstones. International Association of Sedimentology Special Publication, 26, pp. 261–284.Google Scholar
  4. Boles, J.R., and Coombs, D.S., 1975. Mineral reactions in zeolitic Triassic tuff, Hokonui Hills, New Zealand. Geological Society of America Bulletin, 86: 163–173.Google Scholar
  5. Boles, J.R., and Coombs, D.S., 1977. Zeolite facies alteration of sandstone in the Southland syncline, New Zealand. American Journal of Science, 77: 982–1012.Google Scholar
  6. Boles, J.R., and Franks, S.G., 1979. Clay diagenesis in Wilcox sandstones of southwest Texas: Implications of smectite diagenesis on sandstone cementation. Journal of Sedimentary Petrology 49: 55–70.Google Scholar
  7. Boles, J.R., and Ramseyer, K., 1988. Albitization of plagioclase and vitrinite reflectance as paleothermal indicators, San Joaquin Basin. In Graham, S.A. (ed.), Studies of the Geology of the San Joaquin Basin, Pacific Section Society of Economic Paleontologists and Mineralogists, 60, pp. 129–139.Google Scholar
  8. Coombs, D.S., 1954. The nature and alteration of some Triassic sediments from Southland, New Zealand. Transaction of the Royal Society of New Zealand, 82: 65–109.Google Scholar
  9. Curtis, C.D., Coleman, M.L., and Love, L.G., 1986. Pore water evolution during sediment burial from isotopic and mineral chemistry of calcite, dolomite, and siderite. Geochimica et Cosmochimica Acta, 50: 2321–2334.Google Scholar
  10. Hayes, M.J., and Boles, J.R., 1992. Volumetric relations between dissolved plagioclase and kaolinite in sandstones: implications for aluminum mass transfer in the San Joaquin basin, California. Society of Economic Paleontologists and Mineralogists, Special Publication, 47, pp. 110–123.Google Scholar
  11. Hayes, M.J., and Boles, J.R., 1993. Evidence for meteoric recharge in the San Joaquin basin, California provided by isotope and trace element geochemistry. Marine and Petroleum Geology, 10: 135–144.Google Scholar
  12. Heald, M.T., and Larese, R.E., 1974. Influence of coatings on quartz cementation. Journal of Sedimentary Petrology 44: 1269–1274.Google Scholar
  13. Hower, J., Eslinger, E.V., Hower, M.E., and Perry, E.A., 1976. Mechanisms of burial metamorphism of argillaceous sediments: 1. Mineralogic and chemical evidence. Bulletin of the Geological Society of America, 87: 725–737.Google Scholar
  14. Krauskopf, K.B., and Bird, D.K., 1995. Introduction to Geochemistry. 3rd edn., New York, NY: McGraw-Hill Publ. Co., p. 647.Google Scholar
  15. Land, L.S., and Milliken, K.L., 1981. Feldspar diagenesis in the Frio Formation, Brazoria County, Texas Gulf Coast. Geology, 9: 314–318.Google Scholar
  16. Lee, M., Aronson, J.L., and Savin, S.M., 1985. K/Ar dating of gas emplacement in Rotliegendes Sandstone, Netherlands. American Association of Petroleum Geologist Bulletin, 69: 1381–1385.Google Scholar
  17. Mumpton, F.A. (ed.), 1981. Mineralogy and geology of natural zeolites. In Reviews in Mineralogy, 4, Mineralogic Society America, Special Publication, p. 225.Google Scholar
  18. Murata, K.J., and Larson, R.R., 1975. Diagenesis of Miocene siliceous shales, Temblor range, California. U.S. Geological Survey Journal of Research, 3: 553–566.Google Scholar
  19. Pisciotto, K.A., 1980. Diagenetic trends in the siliceous facies Monterey Shale in the Santa Maria region, California. Sedimentology, 28: 547–571.Google Scholar
  20. Ramseyer, K., Diamond, L.W., and Boles, J.R., 1992. Authigenic K-NH4-feldspar in sandstones: a fingerprint of the diagenesis of organic matter. Journal of Sedimentary Petrology, 63: 1092–1099.Google Scholar
  21. Schultz, J.L., Boles, J.R., and Tilton, G.R., 1989. Tracking calcium in the San Joaquin basin, California: a strontium isotopic study of carbonate cements at North Coles Levee. Geochimical et Cosmochimica Acta, 53: 1991–1999.Google Scholar
  22. Stallard, M.L., and Boles, J.R., 1989. Oxygen isotope measurements of albite-quartz-zeolite mineral assemblages, Hokonui Hills, Southland, New Zealand. Clays and Clay Minerals, 37: 409–418.Google Scholar
  23. Thyne, G., and Boles, J.R., 1989. Isotopic evidence for origin of the Moeraki septarian concretions, New Zealand. Journal of Sedimentary Petrology, 59: 272–279.Google Scholar
  24. Walderhaug, O., 1996. Kinetic modeling of quartz cementation and porosity loss in deeply buried sandstone reservoirs. American Association of Petroleum Geologist Bulletin, 80: 731–745.Google Scholar

Cross-references

  1.  Anhydrite and Gypsum  Ankerite Bacteria in Sediments Bentonites and Tonsteins Cathodoluminescence Cements and Cementation Chlorite in Sediments Compaction (Consolidation) of Sediments Diagenesis Diagenetic Structures Dolomite Textures Fabric, Porosity, and Permeability Fluid Inclusions Gases in Sediments Hydrocarbons in Sediments Hydroxides and Oxyhydroxide Minerals Illite Group Clay Minerals Isotopic Methods in Sedimentology Kaolin Group Minerals Magadiite Mixed-Layer Clays Oceanic Sediments Porewaters in Sediments Pressure Solution Sabka, Salt Flats, Salina Seawater Septarian Concretions Siliceous Sediments Smectite Group Sulfide Minerals in Sediments Zeolites in Sedimentary Rocks

Copyright information

© Dowden, Hutchinson & Ross, Inc. 1978

Authors and Affiliations

  • James R. Boles
    • 1
  1. 1.Geological SciencesUniversity of CaliforniaSanta BarbaraUSA